A.A.M.F.R. Smit’s research while affiliated with Wageningen University & Research and other places

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Publications (20)


Fig. 1. WW-Nile arable land vs FAOSTAT arable land estimates (with irrigated area from AQUASTAT). 'Sudan' includes both Sudan and South Sudan, but excludes irrigated area in Sudan.  
Fig. 2. Comparison of WaterWise-Nile runoff contribution and abstraction with modelled runoff (MWRI, 2005) and runoff derived from water balance estimates (Sutcliffe and Parks, 1999) for the main water balance areas of the Nile (in billion m 3 /yr). The water demand of the Delta and Valley was not available for the latter two studies and therefore omitted. No figures for the White Nile are available from Sutcliffe & Parks because of the different catchment schematization. WaterWise-Nile was validated on the wet, average, and dry years of 1999–2001; Sutcliffe and Parks have determined the runoff based on measurement data of the period 1905–1995. The period of the MWRI study represents 1991–2001. Water abstractions of 70 billion M 3 to Egypt support unofficial estimates, suggesting that actual releases at Aswan are higher for the period evaluated than the, often reported, officially allocated 55.5 billion M 3 (Nicol and Cascão, 2011) even after correction for return flows.  
Fig. 3. Increase in annual agricultural gross margin (in USD/ha) between baseline (2005) and 2025 (in a scenario of full " Basin Cooperation " on investments in land use change and water resource allocation for agriculture and hydropower). The regions in dark green represent increase in gross margin in the rehabilitated irrigated areas of Sudan and the new irrigated areas in Ethiopia, under the assumption that they reach the same productivity as Egypt's irrigated areas. The drawn river width is proportional to annual mean discharge in this scenario, with a maximum of 2622 m 3 /s after confluence of the main Nile with the Atbara in Sudan. (For interpretation of the references to colour in this figure legend, the reader is referred to the web version of this article.)  
Fig. 4. Satellite-derived country-specific rainfall (source: Tropical Rainfall Measurement Mission [TRMM] data (Kummerow et al., 1998)) for various spatial delineations for the main cropping seasons (JJASO for Sudan, South Sudan, Ethiopia and Eritrea; MAM and SON for all other countries) in relation to average crop water requirements of rainfed agriculture during these months (set equal to potential crop evapotranspiration, based on average ECMWF reference evapotranspiration (Uppala et al., 2005) and FAO crop factors, see SI). Green shades indicate a range between 75% and 100% of crop water requirements. (For interpretation of the references to colour in this figure legend, the reader is referred to the web version of this article.)  
The role of rainfed agriculture in securing food production in the Nile Basin
  • Article
  • Full-text available

July 2016

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295 Reads

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45 Citations

Environmental Science & Policy

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C.W.J. Roest

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A better use of land and water resources will be necessary to meet the increasing demand for food in the Nile basin. Using a hydro-economic model along the storyline of three future political cooperation scenarios, we show that the future of food production in the Basin lies not in the expansion of intensively irrigated areas and the disputed reallocation of water, but in utilizing the vast forgotten potential of rainfed agriculture in the upstream interior, with supplemental irrigation where needed. Our results indicate that rainfed agriculture can cover more than 75% of the needed increase in food production by the year 2025. Many of the most suitable regions for rainfed agriculture in the Nile basin, however, have been destabilized by recent war and civil unrest. Stabilizing those regions and strengthening intra-basin cooperation via food trade seem to be better strategies than unilateral expansion of upstream irrigation, as the latter will reduce hydropower generation and relocate, rather than increase, food production.

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Pre-Processor KRW-verkenner

January 2014

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11 Reads

De KRW-Verkenner 2.0 is een door Deltares, Alterra en PBL gezamenlijk ontwikkeld model-instrument dat beoogt om de waterbeheerders ondersteuning te bieden bij het opstellen van hun stroomgebied beheersplannen door het verkennen van de effecten van maatregelen (of maatregelpakketten) op de resulterende waterkwaliteit en op de ecologische doelstellingen op het schaalniveau van een waterlichaam. Toepassingen van de Verkenner zijn niet gebonden aan een specifieke ruimtelijke schaal. De eerste toepassing van deze nieuwe versie is in opdracht opgezet als landelijke modeltoepassing met als hoofddoel om de berekende nutriëntenconcentraties aan bemeten oppervlaktewateren te kunnen valideren. Alle datastromen en bewerkingen zijn vastgelegd in een R-script.



RajKumar Frame

December 2013

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518 Reads


Procedure afleiden regionale uit- en afspoelingcijfers voor stikstof en fosfor (herschikkingsprocedure)

January 2013

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5 Reads

De KRW-verkenner, KRW-ECHO zijn voorbeelden van modellen die worden ingezet voor scenariostudies om effecten van bestaand en voorgenomen beleid op de stikstof- en fosforbelasting van het oppervlaktewater in beeld te brengen. Het is gewenst om de diffuse uit- en afspoeling bij regionale toepassingen van de KRW-verkenner en KRW-ECHO te verbeteren.


Calibration of a Distributed Irrigation Water Management Model Using Remotely Sensed Evapotranspiration Rates and Groundwater Head

February 2011

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123 Reads

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25 Citations

Irrigation and Drainage

Parameters of the distributed irrigation water management model FRAME are determined by an inverse method using evapotranspiration (ET) rates estimated from the SEBAL remote sensing procedure and in situ measurement of groundwater heads. The model simulates canal and on-farm water management as well as regional groundwater flow. The calibration is achieved in two phases. The data on ET were introduced with the primary intent of improving predictions of ET through better estimated soil hydraulic parameters. During the first phase, soil hydraulic parameters sensitive to ET were optimized. As per the canal running schedule in the study area, the daily values of ET data were synthesized into 16 time periods with 15 periods each of 24 days and one period of 5 days. Use of cumulative (annual basis) ET data results in better estimates of soil hydraulic parameters as compared to temporal (24-day period basis) ET data due to possible errors in other input data. During the second phase of calibration, aquifer drainable porosity and maximum allowable groundwater extraction were optimized against groundwater heads for five years. The calibration was very successful in about 70% of the study area with a coefficient of correlation between simulated and observed groundwater levels of more than 80%. Subsequently the model is validated against groundwater heads for nine years. Copyright © 2009 John Wiley & Sons, Ltd.



Nutriëntenhuishouding in de bodem en het oppervlaktewater van Quarles van Ufford : bronnen, routes en sturingsmogelijkheden

January 2011

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216 Reads

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3 Citations

Deze rapportage richt zich op het bemalingsgebied Quarles van Ufford. Om zicht te krijgen op de nutriëntenhuishouding in het gebied is er vanaf 2004 aanvullend op het reguliere meetnet van het waterschap in het oppervlaktewater gemeten. Voor de interpretatie van deze meetgegeven en het leggen van relaties om de bronnen en transportroutes van nutriënten in beeld te brengen waren modellen en aanvullende metingen noodzakelijk. In dit synthese-rapport worden de bronnen, routes en de sturingsmogelijkheden om de nutriëntenkwaliteit in het oppervlaktewater van Quarles van Ufford te verbeteren beschreven.


Effect of Model Selection on Computed Water Balance Components

October 2009

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45 Reads

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3 Citations

Irrigation and Drainage

Soil water flow modelling approaches as used in four selected on-farm water management models, namely CROPWAT, FAIDS, CERES and SWAP, are compared through numerical experiments. The soil water simulation approaches used in the first three models are reformulated to incorporate an evapotranspiration process similar to that used in SWAP. Computations are carried out for three soil types, representing sandy loam, loam and sandy clay loam. The reformulated models are calibrated against simulation results obtained with SWAP. All the modelling approaches predict nearly equal estimates of cumulative actual evapotranspiration for a wheat crop. When compared with SWAP simulation results, the CERES type approach outperformed the other two approaches in respect of estimated cumulative deep percolation losses. A new criterion is proposed to interpret simulation results under deep water table conditions to suggest appropriate depth of water application. The resulting recommendations for irrigation planning suggest that any of the modelling approaches may be used to suggest practical irrigation considered in the present study. Copyright © 2008 John Wiley & Sons, Ltd.


Citations (13)


... Rainfall variability and drought are among the most significant threats to developing countries (Damania et al. 2020;Harp et al. 2009;Kinda and Badolo 2019;Lanzafame 2014). In most cases, these countries are heavily reliant on rainfed agriculture (Andersson et al. 2009;Harris and Orr 2014;Siderius et al. 2016), which makes their agricultural systems highly sensitive to climatic fluctuations (Al-Bakri Communicated by H. Babaie et al. 2011;. Specifically, inconsistent rainfall patterns reduce soil moisture during growing periods thereby limiting crop yields and threatening food production (Champagne et al. 2012;Rossato et al. 2017;Tramblay et al. 2011;Varikoden and Revadekar 2018). ...

Reference:

Assessing rainfall variability, long-term trends, and drought incidences in the Tanzania part of the Kagera River sub-basin
The role of rainfed agriculture in securing food production in the Nile Basin

Environmental Science & Policy

... Om meer inzicht te krijgen in de effectiviteit van teeltmaatregelen op verziltende gronden en het belang van de lokale omstandigheden hiervoor, is een case studie (Blom-Zandstra et al., 2014) uitgevoerd voor aardappelteelt. Dit gewas is wereldwijd een zeer belangrijk gewas en volgens trendanalyses van de FAO tot 2050 (World Potato Markets, 2011 2 ) zal de marktpotentie ervan in ontwikkelingslanden snel toenemen. ...

Reference:

Zilte landbouw
Perspectives for the growth of salt tolerant cash crops : a case study with potato

... Change in crop patterns and more efficient irrigation practice is considered as a third measure. Such measures have been promoted and implemented in many water scarce regions (Rhoades et al. 1992;Van Bakel et al. 2009). It can be cost-effective measure with large savings of fresh water, but it is associated with changing farming practices that in many cases have been established over long periods of time, which is not easy. ...

Review of crop salt tolerance in the Netherlands
  • Citing Article
  • January 2009

... uiteen. In het project monitoring stroomgebieden werden percentages gevonden tussen 23 en 59% (Gerven et al., 2011;Roelsma et al., en 2011bSiderius et al., 2011). De Klein en Koelmans (2011) vonden voor dertien West-Europese laaglandrivieren percentages tussen de 39 en 75%. ...

Nutriëntenhuishouding in de bodem en het oppervlaktewater van Quarles van Ufford : bronnen, routes en sturingsmogelijkheden

... Ground experiment or observation methods of ET include the Bowen ratio method and the eddy covariance method (Zheng et al., 2012;Uddin et al., 2013). The model estimation of ET includes a variety of methods such as the FAIDS model, the CERES model, the SWAT model, the SEBAL model, and the CROPWAT model (Eichinger et al., 2006;Jhorar et al., 2009;Zhao et al., 2010;Li and Zhao, 2010;Li et al. 2012Li et al. , 2016bLuo et al., 2012;Miriti et al., 2012;Xiong et al., 2015). Of these, the CROPWAT model is considered to be a reliable model (Zheng et al., 2012;Ismail and Depeweg, 2005) and is provided by the Food and Agriculture Organization (FAO) of the United Nations; it is used to calculate crop water requirement (CWR) (LWD-FAO, 2009). ...

Effect of Model Selection on Computed Water Balance Components
  • Citing Article
  • October 2009

Irrigation and Drainage

... Some hydrological studies utilized remote sensing data before-or a combination of remote sensing and in situ data-to calibrate hydrological models [201][202][203][204][205]. Earlier research demonstrated the capacity to calibrate SWAT with remotely sensed ET data [206][207][208][209][210] and LAI [211,212]. ...

Calibration of a Distributed Irrigation Water Management Model Using Remotely Sensed Evapotranspiration Rates and Groundwater Head
  • Citing Article
  • February 2011

Irrigation and Drainage

... Sementara yang lain menggunakan model simulasi air tanah untuk memprediksi perilaku dinamis dari muka air tanah dalam menanggapi pemompaan air tanah dan pengisian bersih (Omran, 2016). Model pengelolaan air irigasi terdistribusi FRAME, yang merupakan kombinasi dari model aliran tak jenuh SIWARE dan model simulasi air tanah SGMP digunakan untuk studi simulasi (Jhorar et al., 2009 ...

Assessment of alternative water management options for irrigated agriculture
  • Citing Article
  • June 2009

Agricultural Water Management

... For example, the EUROHARP project (Kronvang et al., 2009) compares available distributed models applied in different European countries. The analyzed models span from conceptual models such as NLES_CAT (Simmelsgaard and Djurhuus, 1998) and MONERIS (Behrendt et al., 2003) to more complex and process-oriented models like SWAT and NL-CAT, which are born from the integration of ANIMO (Groenendijk et al., 2005), SWAP (Kroes and Dam, 2003), SWQN (Smit et al., 2009), and SWQL (Siderius et al., 2008). Another example is the GENESIS Project (Groenendijk et al., 2014), which compares 1-D mechanistic models integrating hydrology, vegetation dynamics, and soil biogeochemistry. ...

Process description of SWQN : A simplified hydraulic model

... Michaelis constante voor denitrificatie en de afbraaksnelheid van organische stof) sterk bepalend zijn voor de uitspoeling naar het oppervlaktewater (Jansen et al., 2008;Kroes et al., 2008;Roelsma et al., 2008;. Daarnaast heeft een eerdere gevoeligheidsanalyse aangetoond, dat ook de procesparameters in het oppervlaktewater van grote invloed kunnen zijn, vooral in de poldergebieden ( Van Gerven, 2009 ...

Analyse van de invloed van processen op de nutriëntenconcentraties in het oppervlaktewater : een modelstudie
  • Citing Article
  • January 2009