Article

Land-use/cover changes and their drivers on the slopes of Mount Kilimanjaro, Tanzania

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Abstract

This paper presents the findings of a study that analyzed land use and cover change, their driving forces and the socio-economic implications on the southern and eastern slopes of Mount Kilimanjaro. This study is based on data extracted from remote sensing techniques using 1973, 1984 and 1999/2000 satellite images and household interviews. The major change detected in the study area from satellite images was expansion of cultivation at the expense of natural vegetation. The area under cultivation increased from 54% in 1973 to 62 and 63% in 1984 and 2000, respectively. Expansion and intensification of cultivation were noted particularly in the lowlands while some forest areas in the highlands had become degraded. These changes led to changes in cropping patterns and crop diversification, declined productivity of land and food insecurity. The underlying drivers of these changes were demographic, government policies, economic factors, socio-cultural factors including the land tenure system, institutional factors, technological change and infrastructure development. Investments in irrigation technology, introduction of new crop varieties and government interventions to support the poor are required to improve the productivity of land and reduce the vulnerability of the people to environmental perturbations, including drought.

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... Despite increasing attention investigating the response of vegetation cover to climate change and topographic factors in mountainous regions, relatively few studies have been conducted in tropical mountains (Krishnaswamy et al. 2014;Detsch et al. 2017). There have only been a few bioclimatic studies on Kilimanjaro, Africa's highest mountain at 5895 m above sea level (asl), located in the north-eastern part of Tanzania (Hemp 2009;Torbick et al. 2009;Misana et al. 2012). These studies have demonstrated a substantial shift in vegetation dynamics on the mountain over the past century. ...
... Some studies show a significant correlation between climate patterns and Kilimanjaro's vegetation dynamics using the Normalised Difference Vegetation Index (NDVI) derived from NOAA's Advanced Very High-Resolution Radiometer (AVHRR), with 1 km pixels, and the Global Inventory Monitoring and Modelling System (GIMMS), with 8 km pixels. Most of these studies have examined trends up to 2011 (Torbick et al. 2009;Detsch et al. 2016;Misana et al. 2012). A more recent study by Khalefa et al. (2024), investigated NDVI trends and their driving factors from 2000 to 2022 using NDVI at a much more detailed spatial resolution of (250 m pixels) via the Moderate Resolution Imaging Spectrometer (MODIS). ...
... The dominance of humidity as a predictor in the SW zone highlights its crucial influence on vegetation dynamics. The SW zone of Kilimanjaro is the most densely populated (Misana et al. 2012) and the strong linkage between vegetation health and moisture availability demonstrated here is critical for understanding the wider context of water availability in the cultivated zones (600-1800 m) below the rainforest belt. In recent times, there has been increased variation in water availability both within and between seasons (Agrawala et al. 2003;Hemp 2005), which has increased water stress for communities on the lower slopes (Mckenzie et al. 2010;Misana et al. 2012). ...
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Climatic and topographic factors are critical for influencing vegetation cover, especially in mountainous areas. This study investigates vegetation dynamics in the South‐Western (SW) and North‐Eastern (NE) zones of Kilimanjaro over the past two decades. We used the Moderate Resolution Imaging Spectroradiometer (MODIS) data, focusing on Normalised Differential Vegetation Index (NDVI) trends and their relationship with climatic and topographic factors. The NDVI dataset for 2000–2022 was combined with Digital Elevation Model (DEM) data and corresponding climatic and topographic indices across different elevation zones. Time series analysis shows positive NDVI trends in both zones, with the NE zone exhibiting more significant increases, particularly at lower elevations (665–1800 m), while the SW zone shows positive trends mainly at higher elevations (4000–5000 m). Climatic analysis reveals a complex relationship between NDVI, temperature, and humidity, with the NE zone showing more consistent correlations and the SW zone displaying more variability, especially in the montane forest zone. A Random Forest (RF) regression model highlights the differing importance of climatic and topographic factors: elevation and temperature are the most significant predictors of NDVI in the NE zone, while humidity is the key factor in the SW zone. Overall, these results highlight the differential impacts of climate and topography on vegetation dynamics in the NE and SW zones, reflecting the complex interplay of these factors in influencing vegetation health and distribution. Future work will involve studying the effects of vegetation cover changes and climate heterogeneities on water availability on the slopes of Kilimanjaro to support effective water resource management.
... Favorable weather conditions (good rainfall quantity and distribution) and fertile soil play an important role in crop production, and more than threequarters of the livelihood population of the Kilimanjaro region depends on the resources provided by Mt. Kilimanjaro (Misana et al., 2012;URT, 2017). For more than a century, the majority of farming activities were concentrated in the highlands zone (between 900 and 1800 m above sea level) (URT, 2017). ...
... Smallholder farmers in the highland slopes of Kilimanjaro Mountain have been involved in cultivating the land for over a century and established a very intensive system of land use locally called Kihamba system (tree-banana-coffee system) (Misana et al., 2012); which resembles Kibanja system of Bukoba-northwest of Tanzania (Baijukya et al., 2005). The Kihamba system is multiplelayered, i.e., tree-banana-coffee-grass, which allows nutrient recycling within the system (Misana et al., 2012). ...
... Smallholder farmers in the highland slopes of Kilimanjaro Mountain have been involved in cultivating the land for over a century and established a very intensive system of land use locally called Kihamba system (tree-banana-coffee system) (Misana et al., 2012); which resembles Kibanja system of Bukoba-northwest of Tanzania (Baijukya et al., 2005). The Kihamba system is multiplelayered, i.e., tree-banana-coffee-grass, which allows nutrient recycling within the system (Misana et al., 2012). The intensive multiple cropping together with livestock keeping has stabilized the productivity of the system by providing not only soil cover, which ultimately conserves the soil from erosion, but also the nutrients cycling that has ensured nutrients use efficiently (Ichinose et al., 2019). ...
Article
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In the northern part of Tanzania, the slopes of Mount (Mt.) Kilimanjaro are the most important areas, both in terms of socio-economic development and ecological succession. The main agricultural systems in the area are banana-based (in the highlands) and maize-based (in the lowlands), with strong interlinkage between them via residual transfer from the lowlands to the mountains. This study assessed the soil fertility status between the two contrasting farming areas of highland and lowland farms in Hai district along the slopes of Mt. Kilimanjaro. To achieve this, smallholder farmers along the slope [from above 1000 meters above sea level (m.a.s.l) banana-based down to maize-based, i.e., less than 1000 m.a.s.l] who practice crop residual transfer from maize-based to banana-based farming systems were selected. Qualitative information regarding the demographics, farming practices, and soil fertility management in the two areas were gathered using a semi-structured questionnaire. Soils from both areas (highland and lowland farms) were collected and analyzed in the laboratory for the key soil properties. The demographic results show that agriculture is mostly done by adults and elders (>40 years old). Manure was most commonly reported to be used in the highlands, while inorganic fertilizers were mainly used in lowland areas. The major challenges for soil fertility management are a shortage of manure and high cost of inorganic fertilizers. The results of soil nutrients revealed that lowland zones (>1000 m.a.s.l) had significantly ( p< 0.01) lower levels of nitrogen (0.14%) and organic carbon (OC) (1.22%) compared with highland zones. Extractable phosphorus (P) was significantly lower in both the highland and lowland zones, at 9.3 mg kg ⁻¹ and 8.2 mg kg ⁻¹ , respectively, compared with other nutrients. However, potassium (K ⁺ ) was significantly ( p <0.01) lower [0.34 cmol (+) kg ⁻¹ ] in the highland zone compared to lowland areas. The data show that there is a severe depletion of soil nutrients in the lowland area of Hai district. Notwithstanding the efforts of the small-holder farmers; the study comes to the conclusion that increasing agricultural yield and the sustainability of farming systems require replenishing the nutrients in the soil along the slope of Mount Kilimanjaro.
... The district is divided into Land use in Moshi Rural District is influenced by the altitudinal gradient. The lower area is dominated by maize mono-cropping and pastoralism (Misana et al. 2012). The mid-altitude zones are dominated by mixed farming of trees and crops (home garden agroforestry practice). ...
... The driest period is July through the end of September. The mean annual rainfall is 1000-1200 mm in the lower and mid areas, and 1800-2000 mm in the upper areas (Misana et al. 2012). ...
... The study employed purposive and simple random sampling approaches. Moshi Rural District was purposely selected due to the existence of information on unsustainable water use, and promotion of WCMs (Misana et al. 2012;Kimaro et al. 2019). Within the district, two wards East Old-Moshi and Kimochi were randomly selected out of 31 wards. ...
Article
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Water conservation is necessary to minimize water losses and meet the needs of the growing population. While several domestic water conservation measures (WCMs) have been developed and promoted among households in Africa, the extent of adoption and factors associated with their adoption are not well understood. We conducted an analysis to assess the current level of adoption and identify factors associated with household adoption of domestic WCMs through interviews with 150 randomly selected household heads from six villages in northern Tanzania. On average, 60% of the respondents reported implementing various WCMs whereas 40% did not implement any measures. The most adopted WCM was rainwater harvesting in water tanks, followed by wastewater reuse and the utilization of alternative cleaning methods such as brooms and towels. The likelihood of adopting WCMs was found to be higher among single heads of household compared to married heads of household. Additionally, adoption was negatively correlated with age but positively correlated with the distance between the household's residence and alternative water sources. We recommend targeting water conservation education at elderly individuals, married couples, and those residing near water sources to improve domestic water conservation practices within local communities.
... Campbell et al. (2005) also found that agricultural land was increasing from 7456.64 ha in 1973 to 29,677.22 ha in year 20 0 0, while the forest was decreasing, from 646.34 ha in 1973 to 416.69 ha in 20 0 0, in Kajiado District (western Kilimanjaro, Kenyan side). Similar results were also reported by Misana et al., (2012) . They argued that major changes observed in their study area were the expansion of cultivation down the slopes of Mount Kilimanjaro, where cultivated land replaced natural vegetation. ...
... Transformation of land cover towards cultivated land has been also reported by Chiwa (2012) ; Hemp (2018); IUCN (2003) ; Kalacska et al., (2017) ;Misana, et al., (2012) ;Noe (2003) ;CHIESA project (2015).Chuwa (2013) reported rapid agriculture intensification in the catchment. Misana, et al, (2012) , also reported similar results. ...
... Transformation of land cover towards cultivated land has been also reported by Chiwa (2012) ; Hemp (2018); IUCN (2003) ; Kalacska et al., (2017) ;Misana, et al., (2012) ;Noe (2003) ;CHIESA project (2015).Chuwa (2013) reported rapid agriculture intensification in the catchment. Misana, et al, (2012) , also reported similar results. They observed expansion of land under cultivation down the slopes of Mount Kilimanjaro, where cultivated land replaced natural vegetation. ...
Article
Land use and cover change are closely linked to catchment hydrology characteristics. Land uses and cover determine the ability of the catchment to collect, store, and release water. The catchment water storage and flow ability affect the quantity and timing of runoff, soil erosion, and sediment transport downstream. Agriculture on of the major drivers for the changes in water flow pathways, which also causes a catastrophic shift of aquatic ecosystems. We assessed the impact of land-use changes on the water flow characteristics in the Upper Pangani Sub catchment using the hydrologic model Soil and Water Assessment Tool (SWAT). Land use and cover changes within the Upper Pangani Sub catchment were analyzed between 1987 and 2017 using QGIS. The result shows that agriculture has expanded from 96,737 ha to 314,871 ha between 1987 and 2017. Bare land and built-up land have gained 14690 ha and 7083 ha respectively during this period. Land-use changes have affected the basin's land cover. Forest has decreased from 196558 ha to 106839 ha between 1987 and 2017. Bush land cover has lost 83445 ha during this period. Bushland cover fall victim to agricultural activities, whereas forest is cleared for logging and fire incidences. Consequently, surface runoff has increased from 60.84 to 73.02 (20.6% increase) between 1987 and 2017. Sediment yield has increase from 6.9 to 12.74 ton/ha (46% increase), and groundwater recharge has decreased from 106.53 to 99.56 (6.5% decrease). It concluded that land cover transformation alters hydrology characteristics of the catchment, resulting to fast surface flow, high rate of soil erosion and low infiltration rate. It is recommended that agro-forestry should be emphasized in the catchment.
... Mount Kilimanjaro is the highest free-standing mountain in the world (Newark, 1991) and hosts approximately 2,500 plant and a few hundreds bird species. The classification of its elevational zones is a matter of perspective (Hemp, 2006a;Hemp & Hemp, 2008;Liseki, 2015;Misana, 2012;Soini, 2005a). ...
... Mount Kilimanjaro is home to approximately 1.3 million people (United Republic of Tanzania, 2013), the majority of which lives in the Chagga home gardens (Fernandes et al., 1985). These home gardens are unique, sustainable and well-developed agroforestry systems that have been in use for centuries (Fernandes et al., 1985;Hemp, 2006a;Hemp, 2006b;Misana, 2012;Newark, 1991;Sébastien, 2010;Soini, 2005a). However, over the last decades, these systems have been faced with numerous challenges associated with human population growth and changes in land use (Hemp & Hemp, 2008;Misana, 2012;Sébastien, 2010;Soini, 2005a). ...
... These home gardens are unique, sustainable and well-developed agroforestry systems that have been in use for centuries (Fernandes et al., 1985;Hemp, 2006a;Hemp, 2006b;Misana, 2012;Newark, 1991;Sébastien, 2010;Soini, 2005a). However, over the last decades, these systems have been faced with numerous challenges associated with human population growth and changes in land use (Hemp & Hemp, 2008;Misana, 2012;Sébastien, 2010;Soini, 2005a). ...
Article
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Effective approaches towards sustainability need to be informed by a diverse array of stakeholder perspectives. However, capturing these perspectives in a way that can be integrated with other forms of knowledge can represent a challenge. Here we present the first application of the conceptual framework of the Intergovernmental Science‐Policy Platform on Biodiversity and Ecosystem Services (IPBES) to a participatory assessment of local perspectives on nature, people and sustainability on Mount Kilimanjaro, Tanzania. This assessment was organized in the form of a participatory workshop with five different groups of stakeholders. Following this framework, we assembled information on the state of and trends in species diversity, Nature's Contributions to People (NCP), and on the main drivers of changes in species and habitats. Additionally, we gathered perspectives on the needs and opportunities for the sustainable management and conservation of natural resources from the individual to the international level. The various stakeholders agreed that both the condition and extent of the various habitats and NCP are declining. In line with available knowledge, the key direct drivers of change mentioned by the workshop participants were land use and climate change, whereas human population growth was singled out as the most important indirect driver. The most frequently suggested measures to address the observed decline in species diversity and its drivers were related to land and water management and to education and awareness raising. Yet, the stakeholder groups differed in the measures they suggested. The willingness of a diversity of knowledge holders to systematically engage in a structured discussion around all the elements of the IPBES framework provides support for its applicability in participatory workshops aimed at capturing nuanced and context‐based perspectives on social–ecological systems from informed stakeholders. The application of the IPBES framework enabled the comparability needed for developing narratives of stakeholder visions that can help identify new pathways towards sustainability and guide planning while retaining the context‐based nuances that remain unresolved with non‐participatory methods. Read the free Plain Language Summary for this article on the Journal blog.
... Similarly, mountains of tropical East Africa suffer pressure from growing human populations, opening up of more land for agriculture, and the misuse of natural resources; leading to remarkable changes in its landscapes (Nogués-Bravo et al. 2008). Mostly, LULC changes results from direct and indirect consequences of anthropogenic pushing for natural resources utilization (Misana, Sokoni, and Mbonile 2012). Thus, the growing population among other drivers has increased the vulnerability of the tropical mountains to LULC changes (Kidane, Stahlmann, and Beierkuhnlein 2012). ...
... Kilimanjaro slopes (Munishi, Lema, and Ndakidemi 2015). Reports show rapid expansion in agricultural land along the mountain Kilimanjaro slopes Sokoni 2003, Soini 2005b;Misana, Sokoni, and Mbonile 2012). However, the efforts of the farming community seem to be focused on expanding the farm area aiming at increasing food production. ...
... Several LULC change studies have been done on different spatial and temporal scales on the southern slopes of Mt Kilimanjaro (Mbonile, Misana, and Sokoni 2003;Fairman et al. 2011;Misana, Sokoni, and Mbonile 2012;Mmbaga, Munishi, and Treydte 2017). Conversion of different LULC types to agricultural land on the southern slopes of Mount Kilimanjaro is both historical and a continuous phenomenon. ...
Article
Full-text available
Increasing demand for food production results in Land use and land cover (LULC) changes, which afflicts the provision of ecosystem services in high mountain areas. This work used time-series LULC and selected spatial metrics to predict the LULC changes for Kikafu-Weruweru-Karanga (KWK) watershed (on the southern slopes of Mt. Kilimanjaro) for the next decade. LULC maps were generated by classifying time-series satellite images. We further predicted the implications for selected staple crop production over the next decade. The simulated LULC shows expansion in built-up (by 32.55%/27.04 km 2) and agriculture (by 39.52%/52.0 km2) areas from 2018 to 2030. These results suggest that urbanization is likely the next biggest threat to water availability and food production. Grasslands and wetlands are expected to decrease by 57.24% and 39.29%, respectively. The forest area is likely to shrink by 6.37%, about 9.82 km2, and 1.26 km2 being converted to agriculture and built-up areas, respectively. However, expansion in agricultural land shows very little increase in staple food crop production records, suggesting that farm size plays a minor role in increasing crop production. Predicting the near future LULC around KWK is useful for evaluating the likelihood of achieving development and conservation targets that are set locally, nationally and internationally
... Similarly, mountains of tropical East Africa suffer pressure from growing human populations, opening up of more land for agriculture, and the misuse of natural resources; leading to remarkable changes in its landscapes (Nogués-Bravo et al. 2008). Mostly, LULC changes results from direct and indirect consequences of anthropogenic pushing for natural resources utilization (Misana, Sokoni, and Mbonile 2012). Thus, the growing population among other drivers has increased the vulnerability of the tropical mountains to LULC changes (Kidane, Stahlmann, and Beierkuhnlein 2012). ...
... Kilimanjaro slopes (Munishi, Lema, and Ndakidemi 2015). Reports show rapid expansion in agricultural land along the mountain Kilimanjaro slopes Sokoni 2003, Soini 2005b;Misana, Sokoni, and Mbonile 2012). However, the efforts of the farming community seem to be focused on expanding the farm area aiming at increasing food production. ...
... Several LULC change studies have been done on different spatial and temporal scales on the southern slopes of Mt Kilimanjaro (Mbonile, Misana, and Sokoni 2003;Fairman et al. 2011;Misana, Sokoni, and Mbonile 2012;Mmbaga, Munishi, and Treydte 2017). Conversion of different LULC types to agricultural land on the southern slopes of Mount Kilimanjaro is both historical and a continuous phenomenon. ...
Article
Full-text available
Increasing demand for food production results in Land use and land cover (LULC) changes, which afflicts the provision of ecosystem services in high mountain areas. This work used time-series LULC and selected spatial metrics to predict the LULC changes for Kikafu-Weruweru-Karanga (KWK) watershed (on the southern slopes of Mt. Kilimanjaro) for the next decade. LULC maps were generated by classifying time-series satellite images. We further predicted the implications for selected staple crop production over the next decade. The simulated LULC shows expansion in built-up (by 32.55%/27.04 km2) and agriculture (by 39.52%/52.0 km2) areas from 2018 to 2030. These results suggest that urbanization is likely the next biggest threat to water availability and food production. Grasslands and wetlands are expected to decrease by 57.24% and 39.29%, respectively. The forest area is likely to shrink by 6.37%, about 9.82 km2, and 1.26 km2 being converted to agriculture and built-up areas, respectively. However, expansion in agricultural land shows very little increase in staple food crop production records, suggesting that farm size plays a minor role in increasing crop production. Predicting the near future LULC around KWK is useful for evaluating the likelihood of achieving development and conservation targets that are set locally, nationally and internationally.
... Major land uses in this area are influenced by the altitudinal gradient. The lower area is dominated by maize monocropping and pastoralism (Soini, 2005;Misana et al., 2012). In the mid area (1,200-1,350 m) the dominant farming systems are coffee-banana agroforestry and increasingly also maize fields. ...
... The driest period is from July to end of September, while April and May are the wettest months. The mean annual rainfall increases from 600-900 mm in the lower area, to 1,000-1,200 mm in the mid area and 1,800-2,000 mm in the upper area, respectively (Hemp, 2005;Misana et al., 2012). ...
... The canal network extends over a vast area with variable geomorphologic attributes and land uses (O'Kting'ati, 1991;Devenne, 2006;Misana et al., 2012). For comparison purpose, the study area was subdivided into three sub-regions across the slope, namely: western, central, and eastern parts, respectively. ...
Article
Full-text available
On the southern slopes of Mt.Kilimanjaro like in many other regions in East Africa, agriculture strongly depends on irrigation. Water is supplied to farms by an extensive network of open unlined canals, most of them built centuries ago. However, information about the distribution of these irrigation canals and the dynamics of their discharge is rare thus hampering the implementation of sustainable solutions for agricultural water management. We suppose that several factors like topography, soil properties, shifts of cropping patterns, and weak institutions affect availability and management of agricultural water. Therefore, in this study we determined (i) the distribution of irrigation canals, (ii) their discharge patterns, and (iii) constraints to their sustainable management. Mixed–method approach consisting of both quantitative and qualitative methodologies was used. The discharge of canals was measured at 11 locations along an altitudinal gradient and selected canals were mapped to understanding their distribution, physical characteristics, and potential risks that limits their optimal discharge. Terrain attributes were derived from the Advanced Space borne Thermal Emission and Reflection Radiometer (ASTER) Digital Elevation Model (DEM) and soil physical and hydraulic conductivity were measured to understand permeability and stability of the soil. Additionally, we conducted focus group discussions with participants from 15 villages and 10 key informants interviews. We found that during the dry season the discharge of canals was higher than in the short rainy season. The discharge of canals increased with decreasing elevation. The median daily discharges equaled 12.6, 9.5, and 7.0 l/s in the lower, mid and upper areas, respectively. Landscape in the central part of the study area was the steepest (slope > 60%) and the roughest (Topographic Ruggedness Index > 80 m).We attribute this to terrain heterogeneity across the landscape, thus community decisions about distribution and maintenance of canals could differ across different villages. Furthermore, current shifts of cropping patterns increased irrigation water demands. Both formal and informal water institutions were constrained with several challenges that affected overall management of canals and their sources. Findings of this study could contribute to various efforts dedicated to improve management of water resources around Mt. Kilimanjaro
... Major land uses in this area are influenced by the altitudinal gradient. The lower area is dominated by maize monocropping and pastoralism (Soini, 2005;Misana et al., 2012). In the mid area (1,200-1,350 m) the dominant farming systems are coffee-banana agroforestry and increasingly also maize fields. ...
... The driest period is from July to end of September, while April and May are the wettest months. The mean annual rainfall increases from 600-900 mm in the lower area, to 1,000-1,200 mm in the mid area and 1,800-2,000 mm in the upper area, respectively (Hemp, 2005;Misana et al., 2012). ...
... The canal network extends over a vast area with variable geomorphologic attributes and land uses (O'Kting'ati, 1991;Devenne, 2006;Misana et al., 2012). For comparison purpose, the study area was subdivided into three sub-regions across the slope, namely: western, central, and eastern parts, respectively. ...
Article
Full-text available
On the southern slopes of Mt.Kilimanjaro like in many other regions in East Africa, agriculture strongly depends on irrigation. Water is supplied to farms by an extensive network of open unlined canals, most of them built centuries ago. However, information about the distribution of these irrigation canals and the dynamics of their discharge is rare thus hampering the implementation of sustainable solutions for agricultural water management. We suppose that several factors like topography, soil properties, shifts of cropping patterns, and weak institutions affect availability and management of agricultural water. Therefore, in this study we determined (i) the distribution of irrigation canals, (ii) their discharge patterns, and (iii) constraints to their sustainable management. Mixed–method approach consisting of both quantitative and qualitative methodologies was used. The discharge of canals was measured at 11 locations along an altitudinal gradient and selected canals were mapped to understanding their distribution, physical characteristics, and potential risks that limits their optimal discharge. Terrain attributes were derived from the Advanced Space borne Thermal Emission and Reflection Radiometer (ASTER) Digital Elevation Model (DEM) and soil physical and hydraulic conductivity were measured to understand permeability and stability of the soil. Additionally, we conducted focus group discussions with participants from 15 villages and 10 key informants interviews. We found that during the dry season the discharge of canals was higher than in the short rainy season. The discharge of canals increased with decreasing elevation. The median daily discharges equaled 12.6, 9.5, and 7.0 l/s in the lower, mid and upper areas, respectively. Landscape in the central part of the study area was the steepest (slope > 60%) and the roughest (Topographic Ruggedness Index > 80 m).We attribute this to terrain heterogeneity across the landscape, thus community decisions about distribution and maintenance of canals could differ across different villages. Furthermore, current shifts of cropping patterns increased irrigation water demands. Both formal and informal water institutions were constrained with several challenges that affected overall management of canals and their sources. Findings of this study could contribute to various efforts dedicated to improve management of water resources around Mt. Kilimanjaro.
... Land cover change is complex, involving various interacting factors which vary in space and time (Dalil and Nsini 2014;Misana et al., 2012). On one hand, the variation of factors reflects the dynamic nature of peoples" behavior in the way they interact with their environments, that is, the way they feel, view and respond to their environment in space and time (Orjala, 2008). ...
... Although land cover changes had occurred in the past, they were mostly a result of natural processes and had little effects on the biosphere (Fanan et al., 2011). Recently, the problem has become complex, fast growing, and mostly caused by human activities (Baral et al., 2018;Bayramoğlu and Kadıoğulları, 2018;Mwangi et al., 2017a;Alemayehu, 2016;Dalil and Nsini, 2014;Mdemu et al., 2012;Misana et al., 2012). The major concern on land cover change has emerged following the massive removal of the natural vegetation by human activities (Kull, 2012;Misana et al., 2012). ...
... Recently, the problem has become complex, fast growing, and mostly caused by human activities (Baral et al., 2018;Bayramoğlu and Kadıoğulları, 2018;Mwangi et al., 2017a;Alemayehu, 2016;Dalil and Nsini, 2014;Mdemu et al., 2012;Misana et al., 2012). The major concern on land cover change has emerged following the massive removal of the natural vegetation by human activities (Kull, 2012;Misana et al., 2012). The intensity of changes has been propelled by direct and indirect causes arising from human decisions at global to local levels (Solomon et al., 2018;Mwangi et al., 2017b;Adedeji et al., 2015). ...
... The population of Mt. Kilimanjaro is rapidly growing and almost three quarters of it depends on mountain ecosystem services (Sébastien, 2011;Misana, 2012). However, as in many other parts of the tropics (Perfecto et al., 2009;Karp et al., 2011), the sustainable small-holder agroforestry systems by the local tribe Chagga, who inhabit the area since more than 500 years (Odner, 2010) has been largely transformed by commercial projects in which monocultures with low biodiversity, such as coffee plantations dominate (Maghimbi, 2007). ...
... Kilimanjaro is growing (Sébastien, 2011;Misana, 2012) and if the landscape was further cleared, distances between nesting sites, sites where hymenopterans find food resources and sites where they gather nest-building materials would be too big. Moreover, most of the solitary bees have only short foraging distances of only few hundred meters and remarkably less brood cells are produced with increasing foraging distances (Zurbuchen et al., 2010b;Zurbuchen et al., 2010a). ...
Thesis
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Chapter 1 – General Introduction One of the greatest challenges of ecological research is to predict the response of ecosystems to global change; that is to changes in climate and land use. A complex question in this context is how changing environmental conditions affect ecosystem processes at different levels of communities. To shed light on this issue, I investigate drivers of biodiversity on the level of species richness, functional traits and species interactions in cavity-nesting Hymenoptera. For this purpose, I take advantage of the steep elevational gradient of Mt. Kilimanjaro that shows strong environmental changes on a relatively small spatial scale and thus, provides a good environmental scenario for investigating drivers of diversity. In this thesis, I focus on 1) drivers of species richness at different trophic levels (Chapter 2); 2) seasonal patterns in nest-building activity, life-history traits and ecological rates in three different functional groups and at different elevations (Chapter 3) and 3) changes in cuticular hydrocarbons, pollen composition and microbiomes in Lasioglossum bees caused by climatic variables (Chapter 4). Chapter 2 – Climate and food resources shape species richness and trophic interactions of cavity-nesting Hymenoptera Drivers of species richness have been subject to research for centuries. Temperature, resource availability and top-down regulation as well as the impact of land use are considered to be important factors in determining insect diversity. Yet, the relative importance of each of these factors is unknown. Using trap nests along the elevational gradient of Mt. Kilimanjaro, we tried to disentangle drivers of species richness at different trophic levels. Temperature was the major driver of species richness across trophic levels, with increasing importance of food resources at higher trophic levels in natural antagonists. Parasitism rate was both related to temperature and trophic level, indicating that the relative importance of bottom-up and top-down forces might shift with climate change. Chapter 3 – Seasonal variation in the ecology of tropical cavity-nesting Hymenoptera Natural populations fluctuate with the availability of resources, presence of natural enemies and climatic variations. But tropical mountain seasonality is not yet well investigated. We investigated seasonal patterns in nest-building activity, functional traits and ecological rates in three different insect groups at lower and higher elevations separately. Insects were caught with trap nests which were checked monthly during a 17 months period that included three dry and three rainy seasons. Insects were grouped according to their functional guilds. All groups showed strong seasonality in nest-building activity which was higher and more synchronised among groups at lower elevations. Seasonality in nest building activity of caterpillar-hunting and spider-hunting wasps was linked to climate seasonality while in bees it was strongly linked to the availability of flowers, as well as for the survival rate and sex ratio of bees. Finding adaptations to environmental seasonality might imply that further changes in climatic seasonality by climate change could have an influence on life-history traits of tropical mountain species. Chapter 4 – Cryptic species and hidden ecological interactions of halictine bees along an elevational Gradient Strong environmental gradients such as those occurring along mountain slopes are challenging for species. In this context, hidden adaptations or interactions have rarely been considered. We used bees of the genus Lasioglossum as model organisms because Lasioglossum is the only bee genus occurring with a distribution across the entire elevational gradient at Mt. Kilimanjaro. We asked if and how (a) cuticular hydrocarbons (CHC), which act as a desiccation barrier, change in composition and chain length along with changes in temperature and humidity (b), Lasioglossum bees change their pollen diet with changing resource availability, (c) gut microbiota change with pollen diet and climatic conditions, and surface microbiota change with CHC and climatic conditions, respectively, and if changes are rather influenced by turnover in Lasioglossum species along the elevational gradient. We found physiological adaptations with climate in CHC as well as changes in communities with regard to pollen diet and microbiota, which also correlated with each other. These results suggest that complex interactions and feedbacks among abiotic and biotic conditions determine the species composition in a community. Chapter 5 – General Discussion Abiotic and biotic factors drove species diversity, traits and interactions and they worked differently depending on the functional group that has been studied, and whether spatial or temporal units were considered. It is therefore likely, that in the light of global change, different species, traits and interactions will be affected differently. Furthermore, increasing land use intensity could have additional or interacting effects with climate change on biodiversity, even though the potential land-use effects at Mt. Kilimanjaro are still low and not impairing cavity-nesting Hymenoptera so far. Further studies should address species networks which might reveal more sensitive changes. For that purpose, trap nests provide a good model system to investigate effects of global change on multiple trophic levels and may also reveal direct effects of climate change on entire life-history traits when established under different microclimatic conditions. The non-uniform effects of abiotic and biotic conditions on multiple aspects of biodiversity revealed with this study also highlight that evaluating different aspects of biodiversity can give a more comprehensive picture than single observations.
... Changes in land cover in most of the areas surrounding Mt. Kilimanjaro slopes have the potential to impact water resources [29][30][31][32][33][34]. These changes trigger the need to understand land cover change trajectories and surface-groundwater interaction among the critical requirements in water management practices in the area. ...
... The results show that land cover has changed throughout the study period within the catchment; previous studies also show that land use has changed on the entire slopes of Mt. Kilimanjaro [29,32,33,89,90]. The possible reasons for the escalation of agricultural land and the built-up area may be due to higher population growth rate and socioeconomic development such as the fair prices for horticultural crops in the lowlands. ...
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This study provides a detailed assessment of land cover (LC) changes on the water balance components on data constrained Kikafu-Weruweru-Karanga (KWK) watershed, using the integrated approaches of hydrologic modeling and partial least squares regression (PLSR). The soil and water assessment tool (SWAT) model was validated and used to simulate hydrologic responses of water balance components response to changes in LC in spatial and temporal scale. PLSR was further used to assess the influence of individual LC classes on hydrologic components. PLSR results revealed that expansion in cultivation land and built-up area are the main attributes in the changes in water yield, surface runoff, evapotranspiration (ET), and groundwater flow. The study findings suggest that improving the vegetation cover on the hillside and abandoned land area could help to reduce the direct surface runoff in the KWK watershed, thus, reducing flooding recurring in the area, and that with the ongoing expansion in agricultural land and built-up areas, there will be profound negative impacts in the water balance of the watershed in the near future (2030). This study provides a forecast of the future hydrological parameters in the study area based on changes in land cover if the current land cover changes go unattended. This study provides useful information for the advancement of our policies and practices essential for sustainable water management planning.
... Owing to the fertile soils and favourable climate, the area is densely settled and supports agriculture. The transect has three distinct agro-ecological zones: the highland zone with predominantly coffee and banana cultivation; midlands with predominantly maize and bean growing, and lowlands with dryland agriculture [33]. ...
... Below the Mt. Kilimanjaro National Park, a narrow forest strip was established 1941 as a buffer zone to provide local people with wood and wood products [33]. ...
... For example, around Mt. Kilimanjaro, the average size of land ownership is less than 2 ha per person. is has influenced some households to depend on hired or looking after relatives' land in their absence [73,74]. Given that tenure period is unguaranteed, tenants fear to invest in improving land quality. ...
... e same problem is observed in Mt. Kilimanjaro whereby the Kiamba system involves land passing through sons and thus limits a right of land ownership to women [74]. Comparable findings were reported by Galiè et al. [78] who observed that a lack of gender equality has unnoticed impacts on land management and food security in developing countries. ...
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Agroecosystems are important for food production and conservation of biodiversity while continuing to provide several ecosystem services within the landscape. Despite their economic and ecological benefits, most agroecosystems in Tanzania are degraded at alarming rates. Rapid increase of human population and unprecedented impacts of climate change have influenced depletion of natural resource base within agroecosystem in recent decades compared to what communities have experienced before. Increased food demands owing to population increase have increased pressure on exploitation of land resources including water. Cultivation area and irrigation water demands have increased steadily in the last six decades. Nevertheless, approaches used for water supply have not been improved; thus, water use efficiency in most irrigation schemes is quite poor. Conversely, climate smart agricultural practices are practiced less in Tanzania. There is poor adoption of recommended adaptation among smallholder farmers due to several socioeconomic reasons. One of the key objectives of climate smart agriculture is to improve bio-geochemical interactions within landscape and decrease competition of natural resources between humans and other component of agroecosystems. This underscores the assumptions that most cropping systems in Tanzania are not managed sustainably. Moreover, comprehensive assessment of hydrological dynamics within smallholder farming in Tanzania is highly lacking. Therefore, actual causes and extent of water resources depletion are largely unknown among stakeholders. In most tropical landscapes, water resources degradation is influenced by interaction of both anthropogenic and biophysical factors operating at different times and space scales. As the capacity of water-supplying sources continues to decline, Tanzania needs profound changes in agricultural production systems in order to nourish the growing human population. This calls for strategic approaches that have wider adaptability. A literature survey study with the following objectives was conducted (i) to assess current state of agricultural water use and irrigation activities in Tanzania and (ii) to determine major constraints for sustainable water management and identify appropriate adaptation measures for their improvement across diverse cropping systems.
... Similarly, as in the Taita Hills, the eastern and southern parts receive more rainfall. Mount Kilimanjaro has three distinct agro-ecological zones: the highland zone occurring between 1200 and 1800 m characterized predominantly coffee-banana belt; the midland area, occurring between 900 and 1200 m, is predominantly a maize-bean belt, and; the lowlands that extend 700 to 900 m [33]. A half-mile narrow forest strip occurs above the coffee-banana belt, which was established in 1941 as a buffer forest along the lower edge of the montane forest to provide local people with timber and non-timber forest products, preventing incursion into the National Park [33]. ...
... Mount Kilimanjaro has three distinct agro-ecological zones: the highland zone occurring between 1200 and 1800 m characterized predominantly coffee-banana belt; the midland area, occurring between 900 and 1200 m, is predominantly a maize-bean belt, and; the lowlands that extend 700 to 900 m [33]. A half-mile narrow forest strip occurs above the coffee-banana belt, which was established in 1941 as a buffer forest along the lower edge of the montane forest to provide local people with timber and non-timber forest products, preventing incursion into the National Park [33]. ...
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Mount Kilimanjaro and the Taita Hills are adjacent montane areas that experience similar climate and agricultural activity, but which differ in their geologic history, nature of elevation gradients and cultures. We assessed differences in cropland above ground carbon (AGC) between the two sites and against environmental variables. One hectare sampling plots were randomly distributed along elevational gradients stratified by cropland type; AGC was derived from all trees with diameter ≥ 10 cm at breast height in each plot. Predictor variables were physical and edaphic variables and human population. A generalized linear model was used for predicting AGC with AIC used for ranking models. AGC was spatially upscaled in 2 km buffer and visually compared. Kilimanjaro has higher AGC in cropped and agroforestry areas than the Taita Hills, but only significant difference in AGC variation in agroforestry areas (F = 9.36, p = 0.03). AGC in cropped land and agroforestry in Kilimanjaro has significant difference on mean (t = 4.62, p = 0.001) and variation (F = 17.41, p = 0.007). In the Taita Hills, significant difference is observed only on the mean AGC (t = 4.86, p = 0.001). Common tree species that contribute the most to AGC in Kilimanjaro are Albizia gummifera and Persea americana, and in the Taita Hills Grevillea robusta and Mangifera indica. Significant and univariate predictors of AGC in Mount Kilimanjaro are pH (R2 = 0.80, p = 0.00) and EVI (R2 = 0.68, p = 0.00). On Mount Kilimanjaro, the top multivariate model contained SOC, CEC, pH and BLD (R2 = 0.90, p = 0.00), whereas in the Taita Hills, the top multivariate model contained elevation, slope and population (R2 = 0.89, p = 0.00). Despite of the difference in land management history of Mount Kilimanjaro and the Taita Hills, mean of AGC in croplands does not differ significantly. Difference occurs on variation of AGC, type of trees contributing AGC, and environmental variables that explain AGC distribution. The research results provide reference for management of carbon sequestration on inhabited montane areas. KEYWORDS Aboveground Carbon, Cropland, Agroforestry, Cropped Land, Elevation Gradient
... Simultaneously, extensive land-use change in the densely vegetated foothills accounted for an expansion of cultivated land from 54% in 1973 to 63% in 2000 (Misana et al. 2012) at the expense of natural vegetation (Hemp 2006a)-a trend that seemingly endured beyond the turn of the millennium (Tracewski et al. 2016). While human intervention primarily affects ecosystems outside the protective realms of Kilimanjaro National Park, natural disturbance regimes profoundly modify the upper-mountain vegetation structures. ...
... From a hydrological viewpoint, such massive conversion processes in an area facing a steadily increasing population pressure (Misana et al. 2012) severely affect the regional water cycle, perhaps even more so than climate change (Hardwick et al. 2015). Although an appropriate quantification of land cover-specific water release through ET is of vital importance (Savage 2009), only little data on biosphere-atmosphere water exchange has been available until now. ...
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Future climate characteristics of the southern Kilimanjaro region, Tanzania, are mainly determined by local land-use and global climate change. Reinforcing increasing dryness throughout the twentieth century, ongoing land transformation processes emphasize the need for a proper understanding of the regional-scale water budget and possible implications on related ecosystem functioning and services. Here, we present an analysis of scintillometer-based evapotranspiration (ET) covering seven distinct habitat types across a massive climate gradient from the colline savanna woodlands to the upper-mountain Helichrysum zone (940 to 3960 m.a.s.l.). Random forest-based mean variable importance indicates an outstanding significance of net radiation (Rnet) on the observed ET across all elevation levels. Accordingly, topography and frequent cloud/fog events have a dampening effect at high elevations, whereas no such constraints affect the energy and moisture-rich submontane coffee/grassland level. By contrast, long-term moisture availability is likely to impose restrictions upon evapotranspirative net water loss in savanna, which particularly applies to the pronounced dry season. At plot scale, ET can thereby be approximated reasonably using Rnet, soil heat flux, and to a lesser degree, vapor pressure deficit and rainfall as predictor variables (R² 0.59 to 1.00). While multivariate regression based on pooled meteorological data from all plots proves itself useful for predicting hourly ET rates across a broader range of ecosystems (R² = 0.71), additional gains in explained variance can be achieved when vegetation characteristics as seen from the NDVI are considered (R² = 0.87). To sum up, our results indicate that valuable insights into land cover-specific ET dynamics, including underlying drivers, may be derived even from explicitly short-term measurements in an ecologically highly diverse landscape.
... The anthropogenic biomes surrounding the lake include residential woodland, remote rangeland, residential rangeland, remote croplands, residential rain fed crops, irrigated villages, rain fed villages, pastoral villages, and mixed settlements [37]. Arable land has been increasing in the region since 1973 [48]. The lake is fed by groundwater from Mt. Kilimanjaro and receives on average 565 mm of precipitation, exceeded by surface evaporation estimated at 1735 mm per year [46]. ...
... In an assessment of LUCC for the slopes of Mt. Kilimanjaro, it was indicated that from single date imagery, bushland, grassland and cropland cannot be readily separated due to the transitional nature of the classes and their spectral similarity [48]. Furthermore, vegetation dynamics in the region are strongly influenced by cultivation and land conversion [16]. ...
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Freshwater ecosystems are among the most threatened on Earth, facing environmental and anthropogenic pressures often surpassing their terrestrial counterparts. Land use and land cover change (LUCC) such as degradation and fragmentation of the terrestrial landscape negatively impacts aquatic ecosystems. Satellite imagery allows for an impartial assessment of the past to determine habitat alterations. It can also be used as a forecasting tool in the development of species conservation strategies through models based on ecological factors extracted from imagery. In this study, we analyze Landsat time sequences (1984–2015) to quantify LUCC around three freshwater ecosystems with endemic cichlids in Tanzania. In addition, we examine population growth, agricultural expansion, and climate change as stressors that impact the habitats. We found that the natural vegetation cover surrounding Lake Chala decreased from 15.5% (1984) to 3.5% (2015). At Chemka Springs, we observed a decrease from 7.4% to 3.5% over the same period. While Lake Natron had minimal LUCC, severe climate change impacts have been forecasted for the region. Subsurface water data from the Gravity Recovery and Climate Experiment (GRACE) satellite observations further show a decrease in water resources for the study areas, which could be exacerbated by increased need from a growing population and an increase in agricultural land use.
... Here, we assessed variation in trait composition at the community level and its relationship with above-and belowground organic carbon storage along the large tropical elevational gradient of Mount Kilimanjaro, which ranges from savanna through forest and to the alpine ecosystems. This gradient also encompasses variations in land use, as ecosystems at low to mid-elevation have experienced habitat disturbances and land use transformation (Misana, 2012). We hypothesized that the coordination of belowground and aboveground plant traits at the community level along the climatic gradients of Kilimanjaro matches the primary axes of acquisitive strategies to be found in ecosystems with high precipitation, high land-use intensity and moderate temperature while communities with conservative strategies would be found in ecosystems with low precipitation, and more extreme temperatures (Hypothesis 1). ...
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1. Plant functional traits play an important role in shaping plant ecological responses to environmental conditions and influencing ecosystem functioning. However, how whole-plant functional strategies manifest at the community level to influence aboveground and belowground carbon storage across environmental gradients remains poorly understood. 2. We measured aboveground and belowground carbon stocks and the variation in whole-plant (above- and belowground) functional strategies at the community level in twelve ecosystem types across a broad savanna-forest-alpine elevational gradient of climate and land use on Mt. Kilimanjaro, Tanzania. Using Structural Equation Models, we disentangled the direct and land use mediated influences of climate on carbon storage from indirect influences mediated by variation in plant functional strategies. 3. We found strong coordination between above- and belowground functional traits at the whole community level, which corresponded with functional strategies related to two major trade-offs: a slow -conservation to fast -resource acquisition axis represented by a spectrum from high leaf dry matter content to high fine root nitrogen concentration; and a size-related woody to grassy community axis represented by a spectrum spanning high canopy height to high specific root length. The slow-fast and woody-grassy strategy axes were primarily driven by precipitation and land-use intensity, respectively. 4. Both functional strategies mediated the effects of climate on carbon storage. The slow-fast strategy axis was strongly and positively associated with aboveground carbon stocks. Meanwhile, the woody-grassy strategy axis was negatively associated with both aboveground carbon stocks and soil organic carbon stocks. 5. Synthesis . We demonstrated that major plant functional strategies manifest at the community level along elevational gradients. These strategies also explain variation in carbon storage, although aboveground storage is mostly driven by trait effects, and belowground storage by direct effects of climate. Together, these results underscore the importance of incorporating functional community data into future analysis of climate change impacts on carbon storage, which would enhance our ability to predict potential shifts in ecosystem functioning.
... Moshi Rural District is within the Kilimanjaro region in the northern part of Tanzania, it lies between latitude 2 0 30 ' to 5 0 South and longitude 37 0 to 38 0 East ( Figure 1). The district consists of three belts with different ranges of altitudes which are lowlands 900 m, middle lands 900 -1200 m, and highlands 1200 -1800 m (Misana et al., 2012) and cover a total area of about 1,713 km 2 . The population densities range between 500 -1000 people per km 2 and are found within 1000 and 1800 m altitudes (Hemp, 2006). ...
... It covers the total area of about 1,713 Km 2 . Three belts with different altitude are recognized in the study area, 0 m to 900 m, 900 m to 1200 m and 1200 m to 1800 m altitudes for lowland, middle lands, and highland respectively (Misana et al., 2012). The altitude between 1000 m and 1800 m is highly populated whereby the population densities found to be between 500-1000 peoples per km 2 (Hemp, 2006). ...
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Agroforestry has been widely practiced in the northern highlands of Tanzania because of its prominent effects in reducing soil losses, maintaining soil moisture contents (SMCs), and improving land-use efficiency and farmer’s livelihood. We tested the hypothesis that variations of soil moisture contents in 0-20 cm and 20-40 cm depths from various agroforestry Practices differ significantly in intensified small-scale agroforestry systems. The relationship between SMCs and soil organic carbon was also evaluated. Soil samples were collected from 10 x 10 m2 plot in three points along the diagonal of the quadrat using soil auger. SMCs were determined by gravimetric method and expressed as SMC%. SOC was determined by Walkley and Black method and expressed as SOC %. The variation in SMCs% among the different agroforestry Practices were statistically determined by ANOVA in R software while the correlation between SMCs and SOC were statistically determined by Pearson product-moment analysis. Variation of SMCs was statistically insignificant (p>0.05) among surveyed sites. SMCs increased significantly (p<0.05) with increasing soil depth from 0-40 cm depth in all agroforestry Practices except in the mixed intercropping agroforestry practice (MAP). At 0-20 cm and 20-40 cm, SMCs differed significantly among agroforestry Practices (P = 0.071) and (P = 0.003), respectively. Coffee Intercropping Agroforestry Practice (CIAP) had higher (P<0.05) SMCs at 0-20 cm depth compared to BAP and MWPAP. But, at 20-40 cm depth, soil moisture contents in CIAP differed significantly (P<0.05) with SMCs all AFPs. SMCs showed a positively significant (P<0.05) relationship with SOC within 0-20 cm and 20-40 cm depths. The current study confirms that different agroforestry practices have different influence on the amount and vertical distribution of soil moisture. Therefore, management practices in agroforestry systems should aim to encourage the use of practices which ensure a stable amount of moisture contents in the soil
... On the fertile and densely populated southern slopes of Africa's highest mountain, the Chagga people have lived and shaped the upper part of the territory for more than 400 years with their smallscale "homegarden" farming, while the lower part is characterised by intensive agriculture and urbanised areas, particularly around Moshi [2,4]. Global dynamics, including the growing human population [5,6], evidence of climate change [7,8] and changes in land use and land cover on the slopes [6,[9][10][11][12][13] have impacted the people, their livelihoods and the environment, with water resources being highly affected. ...
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This study assessed the water quality for drinking and irrigation purposes on the southern slopes of Mt. Kilimanjaro during the dry season under low flow conditions. Fifty-one samples covering eight different water sources (i.e., stream water from natural and anthropogenic impacted streams, domestic water, spring water, rainfall, groundwater, lake water and water from irrigation canals) were collected in a snapshot sampling campaign over 10 days in February 2023. First, physical, chemical and biological parameters were analysed and compared with Tanzanian and international drinking and irrigation water quality requirements. The samples were then ranked according to their suitability for drinking and/or irrigation using water quality indices (WQI). All drinking water quality parameters except for E. coli and turbidity were within the permissible limits. A generalised problem of faecal contamination was found in the study area, including in domestic water, highlighting the need to identify sources of contamination and remediate them before distribution. The drinking water quality index (DWQI) classified 89% of the samples as unsuitable and 11% as excellent for drinking. Irrigation water quality parameters were within the guidelines of restriction of use except for pH in 5 samples. In contrast to the DWQI, the vast majority of the water samples (88%) can be used for irrigation without restrictions according to the irrigation water quality index (IWQI). The suitability of water for irrigation was also assessed using three indices, i.e., Kelley’s Index, Soluble Sodium Percentage and Magnesium Ratio, which indicated potential problems with excess of sodium (about 30% of the samples) and magnesium (about 20%). Further studies combining suitability indices, soil characteristics and crop types are recommended to assess water quality for irrigation use.
... Studies conducted upstream of the Pangani River Basin (PRB) where RRB is found, focused on numerous engineering and non-engineering aspects viz., the understanding of the erosion-sediment relationship through SWAT modeling (Ndomba et al. 2007(Ndomba et al. , 2008, the basin hydrological effects due to land use/land cover change (Kiptala et al. 2013;Ouedraogo et al. 2016;Mangi et al. 2022;Said et al. 2021), trend analysis of hydroclimatic variables (Misana et al. 2012;Mmbando and Kleyer 2018;Msigwa et al. 2022), climate change's effects on water resources (Lalika et al. 2015;Munishi and Sawere 2013), and quality-based evaluation of water and its worth in societal uses (Ijumulana et al. 2022;Lyimo et al. 2023;Turpie et al. 2003). ...
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Erosion status resulting from the denudation process in data-limited basins can be achieved through analysis of hydro-morphological parameters. This study aims to the identification of erosion-prone areas using morphometric, hypsometric, and compound factor approaches in the Ruvu River Basin (RRB), Tanzania under a geoinformatics environment. The morphometric and hypsometric parameters were successfully computed. The hypsometric integral (HI) and Compound Factor (CF) ranking techniques were used to assess the erosional vulnerability of the basin. It was found that RRB is a 5th stream order basin having 475 total stream segments and an overall area of 5512.54 km² with a dendritic-type drainage pattern. The bifurcation ratio for the sub-basins from 2.64 to 12 reflects the structural stability of the basin. Drainage density values of 0.121–0.967 km/km² indicate the coarser soil formation, covered by dense vegetation, with low to moderate soil erosion. Results from shape parameters viz.; form factor (0.18–0.441); circularity ratio (0.019–0.424); elongation ratio (0.479–0.749) and compactness ratio (1.536–7.225) indicates sub-basins are elongated in shape, taking moderate lag times for peak runoff to occur, and have low to moderate soil erosion. Ruggedness number (1.625–3.110) confirms that SB1, SB2, SB4, and SB15 are situated in the highly elevated regions of the RRB, and exhibit moderate to steep slopes. These localities have a sturdy influence on intrinsically erosional susceptibility. The hypsometric curve shows the maturity stages of sub-basins and the hypsometric integral exhibits its erosivity in terms of numeric magnitude. Based on both HI and CF prioritization, SB15 has the highest susceptibility to soil erosion followed by SB1 and SB7, ranked 2nd and 3rd respectively. The study proposes that remedial measures, including engineering and non-engineering means, should be considered for SB15 to mitigate soil erosion in the study area.
... Furthermore, application of mechanized agriculture in the district was constrained by smaller sizes of landholdings (<1.5 ha) that were decreasing due to, in part, population growth and application of a customary land tenure system that promoted inheritance of fragmented landholdings by sons. Similarly, an empirical study conducted by Misana et al. (2012) had reported that sociocultural risk factors, including land inheritance by sons, led into smaller land holdings that were less productive in the upper slopes of Mount Kilimanjaro. Consequently, some farmers had to intensify and diversify production in the upper slopes or shift production to the less-fertile lowlands. ...
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Agricultural production systems in semi-arid areas are vulnerable to a myriad of risks. Using a systems approach of risk framework and a mixed-methods research design, this paper sought to explore selected biophysical and socio-economic risks that contributed to vulnerability of agricultural production systems in the semi-arid lowlands of Mwanga District, Kilimanjaro Region, Tanzania. Despite the lack of statistically significant relationships between amounts of rainfall and crop production in the district, 30 focus group participants perceived that spatial and temporal changes of rainfall distribution as coupled with increased crop pest/disease outbreaks and soil loss contributed to vulnerability of agricultural production systems in terms of frequent crop failure and famine particularly amongst farmers who practised rain-fed farming in the semi-arid lowlands. Furthermore, participants perceived that crop production and yields were negatively influenced by poor marketing and institutional structures and that crop production and yields were negatively influenced by farmers’ poor access to appropriate technologies including seeds, fertilizers, agrochemicals, agricultural machinery and infrastructure including modern irrigation schemes and all-weather roads. By way of conclusion, reduced vulnerability of agricultural production systems calls for integrated enhancement of farmers’ capacity in addressing the biophysical, agro-industrial and institutional risks.
... Patterns of LULC were observed to change along the gradient and the later threatened the agricultural land and ecological integrity for elephant habitat, leading to high tension and competition between elephants and people. Misana, 2012 Data extracted from remote sensing techniques using 1973, 1984 and 1999/2000 satellite images and household interviews. ...
... Tree planting increased, especially as boundary planting of exotic species. A similar process took place on Mt Kilimanjaro, particularly after the abolition of chiefs in 1962 (Misana 2012) and private farms were established ( Figure 5.3). In areas such as Kabale in southwest Uganda, there was a progressive conversion of wetlands to cropland, beginning at the wetland margins and progressing to full conversion (Puhalla 2009). ...
Chapter
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The potential for sustainable intensification of highland perennial farming systems in East Africa given the limitations of declining farm size.
... Although the decrease in glaciers corresponds with the previous studies, the cloud cover in the top of the mountain may have influenced the classified image interpretation from which the spectral signatures from the Landsat images obscure the parts of the glacier, thus affecting the training samples as a result and impacting the absolute classification accuracy [59]. [61], the conversion of about 39.5% of bush land to agricultural land between 1973 and 2000 [34], the degradation of more than 41 km 2 of the forest between 1952 and 1982 [62], the conversion of about 49.97 km 2 of shrubs and bush land to agriculture and other uses from 1961 to 2000 in the Kirua Vunjo division [59] and increased cultivated land from 54% (in 1973) to 63% in 2000 on the southern and eastern slopes [63]. ...
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Land use conversion is generally accompanied by large changes in soil organic carbon (SOC). SOC influences soil erodibility through its broad control on aggregate stability, soil structure and infiltration capacity. However, soil erodibility is also influenced by soil properties, clay mineralogy and other human activities. This study aimed to evaluate soil organic carbon as proxy of soil erosion risk in the Nyumba ya Mungu (NYM) catchment in Northern Tanzania. Soil organic carbon (SOC) was measured by an AgroCares scanner from which the soil organic matter (SOM) was derived using the conversional van Bemmelen factor of 1.72. A regression analysis performed between the measured loss on ignition (LOI) values and SOM from the AgroScanner showed a strong positive correlation in all land use classes (LOIFL R2 = 0.85, r = 0.93, p < 0.0001; LOICL R2 = 0.86, r = 0.93, p = 0.0001; LOIGL R2 = 0.68, r = 0.83, p = 0.003; LOIBS R2 = 0.88, r = 0.94, p = 0.0001; LOIBL R2 = 0.83, r = 0.91, p = 0.0002). This indicates that SOC from the soil scanner provided a good representation of the actual SOM present in soils. The study also revealed significant differences in the soil aggregate stability (WSA) and SOM stock between the different land use types in the Upper Pangani Basin. The WSA decreases approximately in the following order: grassland > forest land > bare land > cultivated > bush land. Land use change can thus potentially increase the susceptibility of soil to erosion risk when SOC is reduced. Since WSA was directly related to SOM, the study indicates that, where formal measurements are limited, this simple and inexpensive aggregate stability test can be used by farmers to monitor changes in their soils after management changes and to tentatively assess SOC and soil health.
... Despite this conversion at large scales, production is generally fairly low, particularly in rainfed areas (Nakawuka et al., 2018). Similar observations have been reported from irrigation schemes in northern parts of Tanzania, where expansion of farming has reduced native species (Misana et al., 2012;Said et al., 2021). Brockington et al. (2008) and Rowcroft (2005) reported that agricultural innovation and technologies have transformed much of the habitats beyond their recovery, and still there is a failure to meet production cost in an effective way. ...
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Increasing agricultural land use intensity is one of the major land use/land cover (LULC) changes in wetland ecosystems. LULC changes have major impacts on the environment, livelihoods and nature conservation. In this study, we evaluate the impacts of investments in small-scale irrigation schemes on LULC in relation to regional development in Kilombero Valley, Tanzania. We used Remote Sensing (RS) and Geographical Information System (GIS) techniques together with interviews with Key Informants (KI) and Focus Group Discussion (FGD) with different stakeholders to assess the historical development of irrigation schemes and LULC change at local and regional scales over 3 decades. Overall, LULC differed over time and with spatial scale. The main transformation along irrigation schemes was from grassland and bushland into cultivated land. A similar pattern was also found at the regional valley scale, but here transformations from forest were more common. The rate of expansion of cultivated land was also higher where investments in irrigation infrastructure were made than in the wider valley landscape. While discussing the effects of irrigation and intensification on LULC in the valley, the KI and FGD participants expressed that local investments in intensification and smallholder irrigation may reduce pressure on natural land cover such as forest being transformed into cultivation. Such a pattern of spatially concentrated intensification of land use may provide an opportunity for nature conservation in the valley and likewise contribute positively to increased production and improve livelihoods of smallholder farmers.
... Tree planting increased, especially as boundary planting of exotic species. A similar process took place on Mt Kilimanjaro, particularly after the abolition of chiefs in 1962 (Misana 2012) and private farms were established ( Figure 5.3). In areas such as Kabale in southwest Uganda, there was a progressive conversion of wetlands to cropland, beginning at the wetland margins and progressing to full conversion (Puhalla 2009). ...
Chapter
This book applies a unique, structured, systems methodology for characterizing and grouping large populations of farm households with broadly similar livelihood, production and consumption patterns, and for whom similar development strategies would be appropriate. As a result African households across the continent are grouped into 15 major farming systems and 58subsystems. The farming systems analysis integrates an extensive range of spatial data, administrative statistics, assessment reports and expert knowledge, in order to update the 2001 FAO/World Bank farming systems analysis. Pattern recognition is key to teasing out the diversity inherent to African agriculture and to understanding common livelihood patterns (derived from crops, trees, livestock, fish and off-farm income), constraints and opportunities which define each farming system. The principle of central tendency is used to identify the core length of growing period and travel time to the nearest market town, which are two key indicators of access to agricultural resources and access to agricultural services, respectively, that shape livelihood patterns in each farming system. The method allows farming system drivers, trends and strategic interventions to be identified for policymakers, investors and research planners, using a synthesis of UN statistics, assessment reports and expert knowledge.
... More circumstances at birth surround the wellbeing of the family. Historically, the Rombo-Chagga people developed trade traditions since the penetration of the caravan trades (Rockel 1997) and it is maintained today (Misana et al. 2012). ...
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The history of African societies, which are mostly oral, could be deciphered through onomastics. This is possible because naming practices, which are elaborate, and personal names, which are meaningful, are cherished in African communities. In most cases, the circumstances at birth, which split into several strands, dictate the choice of the name by the name-givers. Naming practice is an elaborate phenomenon amongst the Rombo-Chagga people of Kilimanjaro in Tanzania on two grounds. On the one hand, clan names are associated with Chagga calendar and socioeconomic activities, e.g. Mkenda "born during unlucky days". On the other hand, home-names reveal circumstances at birth and historical events within the family and beyond, e.g. Ndekir"yo"I am cured". In addition, amongst the Bantu speaking communities in Sub-Saharan Africa, naming practices have been influenced by Christianization, Islamicization and colonization. The personal names of the Rombo-Chagga people reveal the strands of religious (formal) names and foreign (English or Kiswahili) names, e.g. Barakaeli "God-bless".
... Tree planting increased, especially as boundary planting of exotic species. A similar process took place on Mt Kilimanjaro, particularly after the abolition of chiefs in 1962 (Misana 2012) and private farms were established ( Figure 5.3). In areas such as Kabale in southwest Uganda, there was a progressive conversion of wetlands to cropland, beginning at the wetland margins and progressing to full conversion (Puhalla 2009). ...
Book
Knowledge of Africa's complex farming systems, set in their socio-economic and environomental context, is an essential ingredient to developing effective strategies for improving food and nutrition security. This book systematically and comprehensively describes the characteristics, trends, drivers of change and strategic prioritiesf or each of Africa's fifteen farming systems and their main subsystems. It shows how a farming systems perspective can be used to identify pathways to household food securiity and poverty reduction, and how strategic interventions may need to differ from one farming system to another. In the analysis, emphasis is placed on understanding farming systems drivers of change, trends and strategic priorities for science and policy. Illustrated with full-colour maps and photographs throughout, the volume provides a comprehensive and insightful analysis of Africa's farming systems and pathways for the future to improve food and nutrition security. The book is an essential follow-up to the seminal work 'Farming Systems and Poverty' by Dixon and colleagues for the Food and Agriculture Organization (FAO) of the United Nations and the World Bank, published in 2001.
... Kilimanjaro with a very broad range of natural and agricultural ecosystems at elevation gradient of approximately 950-2000 m a. s. l. to study the impact of temperature and water availability for various land uses on the enzymes kinetics as a key regulator of nutrient cycling. In Kilimanjaro, agricultural land-use intensification has increased in the past 50 years as a result of increasing population and food demand [23]. Arable soils are consequently modified by mechanization, mineral fertilization and intensive use of pesticides for higher crop yields and pest and disease control [24]. ...
Article
The mobilization of soil nutrients bound in organic matter is largely mediated by enzymes derived from plants, soil microorganisms and animal residues. Land-use change alters important soil characteristics that may affect the activities of soil enzymes. However, mechanistic understanding of how land use and management practices influence the catalytic properties of enzymes in top-and subsoil are still scarce, especially in African ecosystems. We linked catalytic properties i.e. substrate affinity constant (K m) and maximum reaction rate (V max), determined by Michaelis-Menten kinetics, to a set of environmental and microbial variables in the soils of a land-use sequence (6 ecosystems) ranging from natural forests to agricultural fields at Mt. Kilimanjaro. The sensitivity of K m and V max of four extracellular hydrolytical enzymes, β-galactosidase, cellobiohydrolase, phosphatase and chitinase to changing environmental conditions were tested by fluorogenic substrates in topsoils and subsoils. The β-galactosidase activity increased with increasing soil depth. Other extracellular enzyme (cellobiohydrolase, phosphatase and chitinase) activities decreased with depth. The affinity of enzymes to substrates was higher in soils of natural compared to agricultural ecosystems: i.e. higher under forests than under cropland. The activity of β-galactosidase, cellobiohydrolase and chitinase enzyme were highest in lower mountain forest and grassland (less disturbed ecosystems). This indicated that changes in land use and management practice not only affects enzyme activity but also controls enzyme kinetics (K m and K a) thus pointing towards the expression of different enzyme systems. Therefore, we concluded that anthropogenic activities result in alteration of C and nutrient cycling by affecting microbial activities and enzymes catalytic properties.
... Increased water withdrawal is already a serious concern following rapid expansion of cultivation areas, changes in crop types and agronomic practices (Misana et al., 2012;Tagseth, 2008a). Additionally to increased overall food demands, the modern human communities have shifted their food preferences which affects the overall supply chain, production decisions and ultimately quality of landscapes. ...
Article
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The southern slopes of Mt. Kilimanjaro hosts one of the oldest traditional irrigation system in Tanzania, locally known as Mfongo. Today the system is facing several challenges that affect local livelihoods and provision of other ecosystem services. To study the structure of the traditional irrigation systems and its management limitations in the southern slopes of Mt. Kilimanjaro, Tanzania, an interview survey was conducted whereby focus group discussions and key-informants were used as main tools for data collection. Study findings suggest that current water uses under the Mfongo system is not sustainably managed, thus leading to imbalanced water supply among key users. The system is characterized with low water conveyance efficiency and high losses during storage. Disturbances in catchment areas have increased and community participation in canals management has declined. Moreover, poor technical support, conflicting policies and unequal opportunities to land ownership limit local efforts dedicated to improve irrigation activities around Mt. Kilimanjaro. There is an urgent need for technical research on alternative options for agricultural water supply in the area and a need of minimizing water losses from supplying and storage infrastructures.
... It was formed thousands of years ago when lava spilled from the East African Rift Zone and piled around the vent in the shape of the present day three distinct volcanic cones: Kibo the highest peak in Africa at 5,891.8 metres, Mawenzi at 5,149 m and Shira, the shortest cone at 3,962 m. As (Misana et al., 2012) notes, some 1.5 million people live around Mount Kilimanjaro of which nearly three quarters depend on its rich natural resources for their livelihoods, including farming the fertile volcanic soils and many are employed in the mountain's busy tourism industry that sees more than 35 000 climbers a year, plus 5, 000 day visitors (Mitchell et al., 2009) and is one of Tanzania's most important economic sectors (Frömming, 2009 The Drakensberg is also an area of significant anthropological interest, well known for the many ancient San rock paintings that can be found in some 500 caves throughout the region; some of these paintings are possibly as much as 3,000 years old. The Drakensberg is the main watershed of South Africa and is the source of the Orange River. ...
Technical Report
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Th e African Mountains Status Report provides information on the status, trends and levels of threats affecting mountain ecosystems and communities in Africa. The process of compiling this report, started in August 2013 and benefited input from various experts, Mountain Partnership members and specialized institutions in Mountains ecosystems. Special thanks go to SDC for the financial support without which, this report would not have been compiled.
... Kilimanjaro, forest cover degradation increased from 1606 ha in 1973 to 5170 ha in 2000 (Mbonile 2005); the minimum of 41 km 2 was degraded between 1952 and 1982 due to population pressure through building poles, firewood collection and fodder collection (Shishira and Yanda 2001). The southern and eastern slopes also suffer increased cultivated land from 54% (in 1973) to 63% in 2000 (Misana et al. 2012). ...
Article
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This review presents research evidence of climate change and anthropogenic impacts on the slopes of Mt. Kilimanjaro and its implications on water, food and energy production (WFE nexus). While there exist divided scholarly opinions on the impacts of climate change on the Mt. Kilimanjaro glacier, consistent decreases in precipitation amounts are evident throughout the existing literature. The 2050 projections indicate increases in the precipitation amounts by approximately 16–18%. However, it is also stated that there will be a concomitant increase in water deficit of about 71%, 27% and 1% in agriculture, hydropower and livestock production respectively. Despite a large number of researches on impacts of climate and anthropogenic pressure on WFE along Mt. Kilimanjaro slopes, there are still limited long-term, good-quality and high-resolution altitudinal precipitation, temperature records and observation network. Moreover, there is limited information on groundwater recharge areas and their stability under changing environment. It is not clear how the interdependence and interaction between climate change, irrigation, vegetation and river discharges affect groundwater recharge process. Also, there is scarce information on future land use/cover changes. Very limited studies focused on fog water deposition for Mt. Kilimanjaro forest and East Africa, despite its relevance as the water tower of the mountain streams. The review further highlights how both climate and anthropogenic impacts may affect ecosystem services in the region. There is a need for developing adaptive strategies for responding to climate change and anthropogenic impacts on the slopes of Mt. Kilimanjaro now and into the future.
... Farmers in this area practiced more agro-forestry farming (Mmbaga et al., 2017) where banana, coffee and annual crops are intercropped with trees (Fernandes et al., 1985;Mulangu and Kraybill, 2013). Because climates and cropping systems vary with elevation gradient (Misana et al., 2012;Mulangu and Kraybill, 2013;Soini, 2005), insect diversity and composition at different times may differ with different experiences that could lead to different pre and post perceptions of the benefits of these insects. Also, farmers who rely on pollinator dependent crops may have pre existing perceptions about pollinators. ...
Article
Agro-ecological intensification (AEI) harnesses natural processes, such as pollination, that support sustainable crop production and can buffer against future food security risks. However, the transition from conventional agriculture, which relies on inputs that can damage natural ecosystem processes, to more sustainable food production under AEI, is knowledge-intensive. Here, we investigated knowledge gaps among smallholder farmers about pollinators and field margins in a bean agri-system in Tanzania. While 77% of farmers were familiar with and identified honeybees correctly prior to training, only 52% understood their role as a pollinator of crops. Furthermore, 80% and 98% of farmers were unaware of the significance of wild (solitary) bees or the importance of hoverflies as pollinators. A high level of synthetic agrochemical use was reported for the management of pests and weeds, particularly in the more agriculturally intensive production systems. However, an end-line survey conducted one year after training showed an increase in knowledge and the majority of farmers, 99%, 54% and 62% subsequently recognised honeybees, hoverflies and solitary bees respectively, by name. Furthermore, 95%, 69% and 60% of farmers understood the importance of honeybees, hoverflies and solitary bees respectively, as crop pollinators and natural enemies (for hoverflies). Similarly, a majority of farmers recognised the benefits of biopesticides as environmentally safer over synthetic pesticides as well as the value of field margins in supporting pollinators and other ecosystem services. We argue that, improving understanding among smallholder farmers of ecosystem services and their ecological requirements is both feasible and essential to achieving sustainable intensification in small holder farming systems.
... Furthermore, statistically significant decrease of annual rainfall at both Same and NyM Meteorological stations could partly be explained by land-use/land cover changes. In this regard, a study conducted by Misana et al. (2012) in Kilimanjaro Region (also encompassing semi-arid areas in Mwanga District) revealed, through analyses of satellite images dated 1973, 1984 and 1999/2000, expansion of cultivated areas in the southern and eastern lowlands of Mount Kilimanjaro. This was at the expense of natural vegetation, particularly natural forests in the highlands of Mount Kilimanjaro). ...
... For example, Mt. Kilimanjaro region experienced strong land-use intensification within the last 50 years (Misana, Sokoni, & Mbonile, 2012). Despite the risks for ecosystem services, this offers valuable possibilities to study effects of these anthropogenic factors on ecosystem C cycling. ...
Article
Decomposition is one of the most important processes in ecosystem carbon (C) and nutrient cycles, and is a major factor controlling ecosystem functions. The functioning of Afromontane ecosystems and their ability to provide ecosystem services are particularly threatened by climate and land‐use change. Our objectives were to assess the effects of climatic conditions (elevation and seasonality) and land‐use intensity on litter decomposition and C stabilization in ten ecosystems along the unique 3000 m elevation gradient of Mt. Kilimanjaro. Tea‐Bag Index parameters (decomposition‐rate‐constant k and stabilization‐factor S) were used to quantify decomposition of standardized litter substrate. Nine pairs of tea bags (green and rooibos tea) were exposed in each ecosystem during the short‐wet, warm‐dry, long‐wet and cold‐dry season. Decomposition rate increased from k=0.007 in savanna (950 m elevation), up to a maximum of k=0.022 in montane cloud forest (2100 m). This was followed by a 50% decrease in (sub‐)alpine ecosystems (>4000 m). Savanna experienced the strongest seasonal variation, with 23 times higher S‐values in dry season compared to wet season. The conversion of savanna to maize monocultures (~1000 m), and traditional agroforestry to large‐scale coffee plantations (~1300 m) increased mean k‐values, and stabilization factors were about one third lower. Forests between 1900 and 2100 m represent the zone of sufficient moisture and optimal temperature conditions. Seasonal moisture (lower slope) and temperature limitation (alpine zone) decreases litter decomposition. Mt. Kilimanjaro ecosystems are highly sensitive to land‐use change, which accelerates ecosystem cycles and decreases C stabilization.
Article
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Social-ecological systems (SESs) possess a great diversity of land use and land cover (LULC) types with unique assemblages of biodiversity and ecosystem services. However, LULC changes due to landscape fragmentation are emerging as major threats to the system productivity of SESs around the world. This study examined changes to LULC extent and landscape patterns in the Village Tank Cascade Systems (VTCSs) of Sri Lanka using satellite imagery and GIS techniques between 1994 and 2021. Multispectral Landsat images (5 TM and 8 OLI/TIRS) obtained from Google Earth Engine were classified using machine learning algorithms. Overall accuracies obtained were 85.9% (1994) and 88.6% (2021). The LULC change matrix and spatial pattern metrics were used to examine LULC and landscape pattern change dynamics over the VTCS landscapes. LULC change matrix results revealed that forest, which is the dominant LULC class covering 73.7% of the total land area was reduced by 206,725 ha due to transformation into agricultural (70.43%) and scrub (24.33%) lands between 1994 and 2021. Over this time landscape pattern of the VTCS has gradually changed from forest to agricultural land-dominated landscape, with forest and agricultural land types showing a significant negative correlation (p < 0.001; R ² > 0.868), particularly in the southeastern region. Landscape patterns were analysed based on eight spatial metrics calculated at both the landscape and class levels using FRAGSTATS spatial pattern analysis software. At the landscape level, the structure became more dispersed and complex in shape. Heterogeneity was noted to have gradually increased with weakening connectivity, whereas the fragmentation process had gradually accelerated. At the class level, the dominance of forest patches decreased, fragmentation and isolation increased, and connectivity and shape complexity reduced leading to the loss of fragmented forest habitats. The number of patches within the agricultural class increased and became more aggregated and complex in shape. Landscape performance indicators show that VTCSs have experienced a gradual loss of environmental sustainability. Assessment of LULC along with fragmentation can help to monitor the spatial pattern impacts that determine ecological integrity. Thus, the study provides scientific guidance for ecological restoration in degraded VTCSs to effectively improve ecological productivity.
Preprint
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This study assessed the quality of water for drinking and irrigation purposes on the southern slopes of Mt. Kilimanjaro during the dry season under low flow conditions. Fifty-one samples covering 8 different water types were collected in a snapshot sampling campaign over 10 days in February 2023. First, physical, chemical and biological parameters were analysed and compared with Tanzanian and international requirements for drinking and irrigation water quality. The samples were then ranked according to their suitability for drinking and/or irrigation using water quality indices (WQI). All drinking water quality parameters except for E. coli and turbidity were within the reference standards. A generalized problem of faecal contamination was found in the study area, including in domestic water, which highlights the need to identify sources of contamination and remediate before distribution. The drinking water quality index (DWQI) classified 77% of the samples as unsuitable, 4% as poor or very poor and 19% as good or excellent for drinking. Irrigation water quality parameters were within the guidelines of restriction of use except for pH in 5 samples. All samples were classified as safe for irrigation according to the irrigation water quality index (IWQI). However, five other irrigation indices (Kelley’s Index, Soluble Sodium Percentage, Permeability Index, Residual Sodium Bicarbonate and Magnesium Ratio) showed potential problems with excess of sodium and magnesium. A combination of indices is recommended for assessing water quality for irrigation use.
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This paper reviews various aspects of drivers of changing cropping patterns in Nepal based on secondary data sources. Data were acquired from Google Scholar and Research Gate database 32 relevant professional journal articles in between 2000-2022 were intensively reviewed. The drivers of changing cropping patterns are complex and interrelated in the farming system. Spatial analysis of cropping patterns of different geographical scales shows that cropping pattern is an integral part of a behavioral focus to reflect the space relation of the community people. The drivers of changing cropping patterns are numerous and intricately linked. It is challenging to gauge the relative significance of the effects ascribed to each scale of the driver or the interactions between them at any particular geographic region. The study revealed that there are several types of drivers for changing cropping patterns. Among these various types of drivers, the theme of technological advancement/inputs, climate change, infrastructural development, road connectivity, and market demand play prominent roles in changing cropping patterns however other drivers such as off-farm employment, agriculture service extension/training, government policies, population growth/change/migration (rural to urban; international.), are also remarkable in this studies. In the Nepalese context, this study indicates that the more prominent role playing drivers of changing cropping patterns are technological advancement /inputs, infrastructural development and road connectivity, and market demand and climate change however land degradation and government policies also play a role to shifting cropping patterns. These all drivers interact and link with each other, leading to changing cropping patterns in Nepal.
Chapter
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The natural environment is composed of both living and nonliving resources and their interaction dictates the condition of the environment. It provides food, shelter, economic returns, food source, and sustenance to diverse biota. The major components of the environment are the mountains, aquatic bodies, forests, and grasslands which provide a haven for diverse species of animals. Some of these components and areas serve as travel and tourist destinations, thereby providing foreign exchange which results in economic growth. The Northern African regions are well-established in these activities when compared with the sub-Saharan regions of Africa. These regions have potentials that can be exploited for revenue generation if policies are created to harness these resources. The synergy between atmospheric, water, and mineral resources in the environment must be preserved to enjoy the use and non-use benefits. Although, these resources are affected by human pressures in the form of overharvesting of natural resources, changes in a habitat-like fragmentation and modification, and the introduction of invasive alien species. Measures such as good governance and community participation by locals are important in resource management. To this end, this chapter reviews the environmental resources and approaches for sustainability.KeywordsNatural resourcesSustainabilityHuman populationEnvironmental policyCommunity participation
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This paper analyses long-term and incremental land use changes that have taken place in Mount Rungwe ecosystem in Tanzania from 1973 to 2010 basing on information derived from satellite images, household socio-economic data, focus group discussions and interviews with key informants. While most literature on land use change reports negative effects, land use changes in Mount Rungwe ecosystem have positively benefited communities through more diversification and greater commercialisation. The paper demonstrates that rural communities’ livelihoods are both a cause and a result of changes in the natural Mount Rungwe ecosystem. The changes in land use through cropping patterns and reforestation took advantage of opportunities from population increase, access to markets and agricultural resources management. Consequently, the changes have qualitatively improved communities’ livelihoods and forest ecosystems. The paper broadens our understanding on the potential land use changes in mountain ecosystems for enhancing rural livelihoods and the environment in line with the Boserup’s agricultural intensification theory.
Article
Anthropogenic modification of montane forests to other land uses has significant effects on native vegetation and the ecological functions of plant communities, such as in the forests of Mount Kilimanjaro. This study was carried out in Kilimanjaro National Park at the former Engushai forest village, where local people were relocated for conservation in 2006. Forty 20 × 50 m plots were established in areas with different historical land use (former settlement, former cultivation, transition and natural forest). We recorded 132 plant species, representing 114 genera and 58 families. The highest tree species richness was recorded in the forest zone (11 ± 1 per plot), followed by in the transition zone (7 ± 1), former cultivation zone (4 ± 1) and former settlement zone (4 ± 0.4). The natural forest was more diverse in terms of tree species than other sites (H’ = 1.83 ± 0.09, evenness of 0.48 ± 0.02). Analysis of variance showed significant variation in tree species richness, diversity index and evenness among previously disturbed sites and natural forests. The vegetation is at an early stage of succession in anthropogenically impacted areas. However, the domination of Vernonia lasiopus and Bothriocline longipes in the formerly degraded areas was crucial for restoring the microclimate and soil fertility vital for forest development. There is adequate potential for and patterns of natural regeneration of indigenous trees in the anthropogenically impacted areas. The current passive management by Kilimanjaro National Park facilitates forest recovery, indicating the high resilience of these montane forests. It is recommended to monitor the future recovery and succession of the lower montane forest.
Chapter
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The overwhelming demand of deadwoods outside protected areas has not given deadwoods enough time to remain standing for the formation of the tree cavities by birds and other natural agents. Consequently, cavity adopter and large-bodied species face difficulties in finding and establishing acceptable nest sites. The focus of biodiversity conservation has been mainly within protected area systems, and less attention has been given to areas outside protected areas despite the fact that these areas support a bigger proportion of bird community. A high pace of deadwood loss on the entire landscape on the southern slopes of Mount Kilimanjaro is an irreversible situation in which is increasingly becoming a growing concern for the conservation of biodiversity beyond protected areas. Here, we investigate what extent deadwoods have in providing nest sites among cavity-nesting birds. We do this through observations and by placing artificial nest boxes on trees within three different land-use types. We found that deadwood volume and number of natural tree cavities were lower at coffee plantations as compared to mixed farming areas and Kilimanjaro National Park (KINAPA). Likewise, tree cavity positions from the ground were higher at coffee plantations than in other two land-use types. However, application of artificial nest boxes reveals that a good number of larger artificial nest boxes had greater occupancy, as did boxes placed at higher positions on trees from the ground at coffee plantations and mixed farming areas than at KINAPA, suggesting a shortage of natural cavity-nesting sites for larger birds and an avoidance of nest predation or human disturbances, respectively. Therefore, provision of artificial nest boxes could offer nesting opportunities for a range of cavity-nesting birds if designs and constructions take into consideration all possible factors that might hinder their occupation by cavity-nesting birds. In this manner, application of cavity nest boxes could be a vital alternative tool for conservation of cavity-nesting birds beyond boundaries of protected areas.
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Background Land use/cover (LULC) change is a dynamic and complex process that can be caused by many interacting processes ranging from various natural factors to socioeconomic dynamics . It exerts a strong influence on the structure, functions and dynamics of most landscapes. Monitoring and mapping of LULC dynamics are crucial as changes observed reflect the status of the environment and provide input parameters for optimum natural resources management and utilization. The objective of this study was to quantify the spatio-temporal LULC dynamics using satellite image coupled with local perceptions in the Gedalas watershed of the Blue Nile Basin, North Eastern Ethiopia. Maximum likelihood supervised image classification technique were employed to classify LULC categories. After ensuring acceptable accuracy value for each classified image, image differencing approach was used to detect and quantify LULC transitions of the area. Classification results were validated with the aid of field work, topographic maps, and high resolution Google earth images supplemented with other available thematic data sets. The results The result demonstrated seven major LULC classes and the overall scenario presented by the study reveals that the watershed has experienced quite visible LULC transitions that seem to be continued in the future due to eternal anthropogenic activities and natural factors. The study ascertain that though there was change in all land use types, the major change detected was a consistent expansion of farmland/settlements area mainly at the expense of Afro/sub Afro alpine vegetation areas. On the contrary, Afro/sub Afro alpine vegetation showed a consistent net loss of over the study of periods. The findings also highlighted that transitions were ultimately driven by the interplay of biophysical, socioeconomic and institutional factors. Perceptions of the local communities on the LULC change substantially agree with data from satellite images. This implies that the ongoing rural land administration and natural resource conservation and management strategies could not effectively address the expansion of agricultural land towards fragile and marginal lands in the study area. Conclusion The study concludes that if these trends of crop lands expansion allowed continuing, sooner or later there will be no Afro/sub Afro alpine vegetation will remain. Therefore, local governments should strive to expand SLM activities on such mountain ecosystems and other marginal lands focusing on community livelihood diversification and sustainable intensification strategies.
Poster
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Traditional irrigation canals play important role in stabilizing agricultural production and other biogeochemical ecosystem processes around Mt. Kilimanjaro. However, number of factors have been reported to affect its discharge and we are currently lacking a clear understanding of the actual causes and extent of the problem We suspect that socio-economic aspect of agricultural water use is likely to contribute to this problem. This forms a basis of this study.
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We highlight the complexity of land-use/cover change and propose a framework for a more general understanding of the issue, with emphasis on tropical regions. The review summarizes recent estimates on changes in cropland, agricul-tural intensification, tropical deforestation, pasture expansion, and urbanization and identifies the still unmeasured land-cover changes. Climate-driven land-cover mod-ifications interact with land-use changes. Land-use change is driven by synergetic factor combinations of resource scarcity leading to an increase in the pressure of production on resources, changing opportunities created by markets, outside policy intervention, loss of adaptive capacity, and changes in social organization and atti-tudes. The changes in ecosystem goods and services that result from land-use change feed back on the drivers of land-use change. A restricted set of dominant pathways of land-use change is identified. Land-use change can be understood using the con-cepts of complex adaptive systems and transitions. Integrated, place-based research on land-use/land-cover change requires a combination of the agent-based systems and nar-rative perspectives of understanding. We argue in this paper that a systematic analysis of local-scale land-use change studies, conducted over a range of timescales, helps to uncover general principles that provide an explanation and prediction of new land-use changes.
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Since time immemorial, humankind has changed landscapes in attempts to improve the amount, quality, and security of natural resources critical to its well being, such as food, freshwater, fiber, and medicinal products. Through the increased use of innovation, human populations have, slowly at first, and at increasingly rapid pace later on, increased its ability to derive resources from the environment, and expand its territory. Several authors have identified three different phases - the control of fire, domestication of biota, and fossil-fuel use - as being pivotal in enabling increased appropriation of natural resources (Goudsblom and De Vries 2004; Turner II and McCandless 2004).
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(voir l'ouvrage édité en langue française en 2003 Kilimandjaro : montagne, mémoire, modernité. Pessac (France) : Presses Universitaires de Bordeaux, 2003. 366 p.ISBN 2-906621-31-5)
Article
Mount Kilimanjaro (5,896 m) in northeastern Tanzania is a huge volcanic cone the slopes of which are well endowed with fertile volcanic soils and abundant rainfall. They have supported an unusually dense population which increased from 128,000 in 1921 to 694,000 in 1978, and most of the people are concentrated in the wet highlands above 900 m. This created a land shortage and the average farm size decreased to one-tenth of that in 1921. The farmers were forced to diversify crops and intensify land use, and the carrying capacity of the land was more than doubled. Resource management techniques included terracing, irrigation, application of manure and fertilizer, and maintenance of shade trees to reduce soil erosion. Labour input per unit doubled between the 1930s and 1970; grazing lands and river valleys in the highlands were planted with coffee and bananas; and people settled in the dry lowlands to grow maize and cotton and to raise livestock. Further intensification by the introduction of dairying and cardamom growing may raise the carrying capacity, and the government has introduced new policies (irrigation, small-scale rural industries, outmigration) to try to maintain some stability and to correct the growing imbalance between resources and population in Kilimanjaro. /// Le Mont Kilimanjaro (5.896 m) dans le nord-est de la Tanzanie est un immense cône volcanique dont les versants sont recouverts de riches sols volcaniques recevant des pluies abondantes. En conséquence, la population a rapidement augmenté, de 128.000 habitants en 1921 à 694.000 en 1978, les plus hautes concentrations se trouvant dans les hautes terres humides au-dessus de 900 m. Un manque de terres disponibles s'est manifesté, si bien que la taille moyenne des fermes est maintenant un dixième de ce qu'elle était en 1921. Les agriculteurs ont été obligés de diversifier leurs cultures et d'intensifier l'exploitation du sol; la charge globale a plus que doublé. Des techniques de gestion des ressources ont été appliquées pour réduire l'érosion du sol, y compris la construction de terrasses, l'irrigation, l'application de fumier et d'engrais, ansi que la plantation d'essences d'ombre. La main d'oeuvre disponible par unité de surface a doublé entre 1930 et 1970, les pâturages et les vallées des hautes terres ont été plantées avec des caféiers et des bananiers, et la population s'est étabile dans les basses terres sèches pour cultiver du maïs et du coton et élever du bétail. Une plus grande intensification par l'introduction de l'élevage laitier et de la culture du cardamome pourrait encore augmenter la charge globale, et le gouvernement a pris de nouvelles mesures (irrigation, industries rurales à petite échelle, migration en dehors de la région) pour essayer de maintenir une certaine stabilité et de rectifier le déséquilibre croissant entre les ressources et la population du Kilimanjaro. /// Der Kilimanscharo (5.896 m) in Nordost Tansania ist ein riesiger vulkanischer Kegelberg, dessen fruchtbare Hänge ausreichend Niederschläge erhalten. Dieses Ackerland versorgte eine ungewöhnlich große Bevölkerung, die von 128.000 im Jahre 1921 auf 694.000 im Jahre 1978 anwuchs. Die Besiedelung konzentrierte sich auf die feuchten Hochländer oberhalb 900 m, was zu Landverknappung führte. Die durchschnittliche Größe eines landwirtschaftlichen Betriebes verringerte sich auf 1/10 der Größe von 1921. Die Bauern waren gezwungen, Mischkulturen anzubauen, und die Landnutzung zu intensivieren, wodurch sich die Ertragsfähigkeit verdoppelte. Ressource-Managementmethoden wie Terrassierung, Bewässerung, Anwendung von Natur-und Kunstdünger und Erhaltung von Schattenbäumen zur Reduzierung der Bodenerosion wurden angewendet. Zwischen 1930 und 1970 verdoppelte sich der Arbeitsaufwand pro Fläche; Weideflächen und Talgründe in den Hochländern wurden mit Kaffee und Bananen bepflanzt; Menschen siedelten in den trockenen Tieflanden, um Mais und Baumwolle anzubauen und Viehzucht zu betreiben. Eine weitere Intensivierung durch Einfuhr von Milchkühen und Kardamomanbau könnte die Ertragsfähigkeit erhöhen; daneben hat Regierungspolitik (z.B. Bewässerung, kleinbäuerliche Industrien, Abwanderung) dazu beigetragen, eine gewisse Stabilität aufrechtzuerhalten und das wachsende Ungleichgewicht zwischen Ressourcen und der Bevölkerungsdichte am Kilimanscharo auszugleichen.
Article
Human actions are altering the terrestrial environment at unprecedented rates, magnitudes, and spatial scales. Land-cover change stemming from human and uses represents a major source and a major element of global environmental change. An international and interdisciplinary agenda is currently being developed to address these issues, through several closely-connected foci of study. A division of the world according to common situations of environment, human driving forces, and land-cover dynamics will be followed by detailed study of the processes at work within each situation. The results will form the basis for a concurrent effort to develop a global land model that can offer projections of patterns of land transformation. -from Authors
Article
Mountains are complex and fragile ecosystems characterised by vertically, highly differentiated climatic conditions and often by an abundance of water and rich biodiversity. Mountains are high-risk environments: avalanches, glacial lake outbursts, landslides and earthquakes threaten life in mountain areas. Remoteness and difficult access hamper development in mountain regions. Therefore, mountain areas are often marginalized. Despite these constraints, mountains offer significant opportunities. Mountain dwellers have adapted to life in steep and harsh conditions and have developed sophisticated techniques for farming, water use, forestry and communication. The agro-biodiversity as a function of altitude, exposition and farmers’ crop selection is huge. Mountain inhabitants have also developed a rich cultural diversity. Therefore, people living in lowland areas or in big cities increasingly prefer mountains for recreation.
Chapter
Concerns about land-use/cover change emerged in the research agenda on global environmental change several decades ago with the realization that land-surface processes influence climate. In the mid-1970s, it was recognized that land-cover change modifies surface albedo and thus surfaceatmosphere energy exchanges, which have an impact on regional climate (Otterman 1974; Charney and Stone 1975; Sagan et al. 1979). In the early 1980s, terrestrial ecosystems as sources and sinks of carbon were highlighted; this underscored the impact of land-use/cover change on global climate via carbon cycle (Woodwell et al. 1983; Houghton et al. 1985). Decreasing the uncertainty of these terrestrial sources and sinks of carbon remains a serious challenge today. Subsequently, the important contribution of local evapotranspiration to the water cycle – that is, precipitation recycling – as a function of land cover highlighted yet another considerable impact of land-use/cover change on climate, at a local to regional scale in this case (Eltahir and Bras 1996).
Chapter
One of the key activities of the Land-Use/Cover Change (LUCC) project has been to stimulate the syntheses of knowledge of land-use/cover change processes, and in particular to advance understanding of the causes of land change (see Chap. 1). Such efforts have generally followed one of two approaches: broad scale cross-sectional analyses (cross-national statistical comparisons, mainly); and detailed case studies at the local scale. The LUCC project applied a middle path that combines the richness of indepth case studies with the power of generalization gained from larger samples, thus drawing upon the strengths of both approaches. In particular, systematic comparative analyses of published case studies on landuse dynamics have helped to improve our knowledge about causes of land-use change. Principally, two methods exist for comparative analyses of case studies. These methods are sufficiently broad geographically to support generalization, but at a scale fine enough to capture complexity and variability across space and time.
Article
The homegardens are characterised by an intensive integration of numerous multipurpose trees and shrubs with food crops and animals, simultaneously on the same unit of land. The Chagga are skilled farmers with an intimate knowledge of the crops and their ecological requirements. They have a good idea of functions/uses of the plant species on their farms. The large species diversity provides both subsistence and cash crops. It enables the farmer to keep his management options open and provides insurance against drought, pest and economic risks.
Article
This study is about changes in land use and interactions of land use change and livelihoods in the Chagga farming system on the slopes of Mt. Kilimanjaro, Tanzania. An aerial photo interpretation and fragmentation analysis of the years 1961, 1982 and 2000 was conducted covering approximately the Kirua Vunjo Division, a transect of 152 km2 from the forest reserve edge to the plains. Earlier changes were traced from literature review. The results show the expansion of cultivation to more marginal land down the slope, the disappearance and extreme fragmentation of bush land and appearance and expansion of settlements. The home garden area has experienced some specific internal change, but has not expanded down the slope. In the 1960s there were small open fields and patches of grazing lands amongst home gardens. In the 1980s the area was more uniformly covered by homegardens. Since then it has become patchy again as new homesteads have been built on subdivided farms and more food is produced on the higher slopes. Population pressure and the ensuing expansion of agriculture to more marginal land, intensification of the homegarden system, together with climate changes affecting the water supplies, have caused changes in farmers’ livelihoods. As land scarcity now hinders expansion of agriculture, farm size has seriously decreased, common resources have become scarce, and prices of coffee in the world market remain low, farmers are trying to intensify and diversify their farm production. Local initiative is leading to change, but the locally conceived alternatives are too few and lack integrated approaches of technical agricultural research, economic analysis, and policy studies and reforms. Non-agricultural activities and paid employment are becoming increasingly important. However, due to considerable entry barriers to remunerable off-farm jobs, not all households enjoy equal access to attractive non-farm opportunities. The future welfare of the area will depend on increasing the marketable knowledge and skills of the population that will enable it to become integrated in the economy of the region and the country.
Article
Clarification of several issues in the human dimensions of global environmental change is essential to the creation of a balanced research agenda. Global environmental change includes both systemic changes that operate globally through the major systems of the geosphere-biosphere, and cumulative changes that represent the global accumulation of localized changes. An understanding of the human dimen sions of change requires attention to both types through research that integrates findings from spatial scales ranging from the global to the local. A regional or meso-scale focus represents a particularly promising avenue of approach.
Article
Using a meta-analytical research design, we analyzed subnational case studies (n = 132) on the causes of dryland degradation, also referred to as desertification, to determine whether the proximate causes and underlying driving forces fall into any pattern and to identify mediating factors, feedback mechanisms, cross-scalar dynamics, and typical pathways of dryland ecosystem change. Our results show that desertification is driven by a limited suite of recurrent core variables, of which the most prominent at the underlying level are climatic factors, economic factors, institutions, national policies, population growth, and remote influences. At the proximate level, these factors drive cropland expansion, overgrazing, and infrastructure extension. Identifiable regional patterns of synergies among causal factors, in combination with feedback mechanisms and regional land-use and environmental histories, make up specific pathways of land change for each region and time period. Understanding these pathways is crucial for appropriate policy interventions, which have to be fine-tuned to the region-specific dynamic patterns associated with desertification.
Article
Peasant households in Tanzania have a variety of income sources. However, establishing a crop in the peasant farming culture requires much investment, and the decline of a crop that is a source of livelihood can cause much misery. Widespread social and economic changes in the peasant society and in the regional society as a whole have led to a decline in coffee crops in Kilimanjaro since the 1970s, despite the fact that coffee is its principal cash crop. This paper explores the decline of coffee and the ascendancy of rice and maize as major crops in the Kilimanjaro region. The driving forces behind these changes in crop culture are considered. The argument is made that wider institutional changes, in addition to internal changes in peasant households, have contributed to the decline of coffee and the rise of maize and rice as the principal crops.
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