Quinquennia drought duration in Europe between 1969 and 2018

Quinquennia drought duration in Europe between 1969 and 2018

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The questions of scale, limit, and areal extent are central points for any drought assessment effort. Drought indices, such as the Standardized Precipitation Index (SPI) and the Standardized Precipitation Evapotranspiration Index (SPEI), are assisting to demarcate drought characteristics and spatial extent. The current approach utilizes the E-OBS g...

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... Numerous studies have examined how drought changes (Tsakiris et al., 2008;Azimi et al., 2020;Oikonomou et al., 2020;Tatli et al. 2020;Topcu & Seckin, 2021;Motavali Bashi Naeini et al. 2021;Kamali & Asghari, 2022;Chisadza et al., 2023;Achite et al., 2023). This studies considered different drought indices and discussed the ability of each. ...
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... Evidence of all this was observed in 2011, a year of particularly intense agricultural drought in the German regions (Figure 4), causing an average yield reduction of more than 9% in cereals (Table 4). This result is consistent with that of [142], which classified the 2011 drought in the EU as having the largest spatial extent on record. In the same context, [115] studied droughts using meteorological indices for southwestern Germany and classified 2011 as one of the most extreme years with precipitation shortages accompanied by high temperatures. ...
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... Beavers are semi-aquatic rodents that need water throughout the year; feeding and other activity mostly occurs within 20 m of the water edge (Gaywood, 2018). Therefore, severe droughts in warm months as those occurring in southern Europe are major limiting factors (Zavyalov et al., 2015;Oikonomou et al., 2020;Sutanto et al., 2020;Serva, Biondi, & Iannella, 2023). Similarly, in Italy, suitability was low in areas with cold climates (e.g. the Alps) or with warm and dry Mediterranean climates (e.g. ...
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... Among the other authors who focused their studies on SPEI in the conditions of European climate, [25] (Serbia) and [26] (Europe) decided to use GEV in their work, while [27] (Czech Republic); [17] (Europe); [28] (Europe); [29] (six European sites located in midlatitudes); and [30] (Europe) followed the Log-logistic distribution. ...
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... Characterization of drought is necessary for the planning of various activities in the economy, industry, or water sector in general. Drought and spatial distribution of drought events in Europe were characterized by Oikonomou et al. (2020). ...
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... Given the climate expected in the near future, a more frequent summer drought will occur in Europe [2,40], one of the major yield-limiting climate factors [41]. Drought is an abiotic factor that causes significant yield losses, especially in rain-fed agriculture. ...
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... An SPI3 selection depicts eastern Europe and increasing tendencies over southern and eastern Europe, while central Europe and some parts of eastern Europe represent the transition zone. On the contrary, using monthly steps above 6 months depicts more drought events in central and northern Europe [26,[51][52][53][54][55]. ...
... Using this drought index with 6-and 12-month scales may demonstrate irregular water resources and extremely low-level reservoir storage (hydrological droughts) [7,26,40,56,57]. For every climatic zone in Europe, SPI values of time scales of 6 months or above are more suitable for drought characterization than time scales of 3 months or below. ...
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The ever-increasing need for water, the alteration in the climate, and its observed changes over recent years have triggered a lot of research studies associated with the phenomenon of drought. Within the wider geographical region of the Mediterranean, the relevant scientific subject seems to be of great interest, since it is undoubtedly related to a number of severe socio-economic consequences. This present effort focuses on the evolution of this particular phenomenon over time, within the borders of nine different countries in the Eastern Mediterranean (Athens, Greece—Europe; Constantinople, Turkey—Asia; Nicosia, Cyprus—Europe; Jerusalem, Israel—Asia; Amman, Jordan—Asia; Damascus, Syria—Asia; Beirut, Lebanon—Asia; Cairo, Egypt—Africa; and Tripoli Libya—Africa). By applying the Standard Precipitation Index (SPI), examining precipitation data at the month level (January 1901 to December 2020), and utilizing the Inverse Distance Weighted (IDW) method, the spatio–temporal variability of drought events in the Eastern Mediterranean area was studied. In Jerusalem, long-term droughts presented a higher than usual volume, in accordance with applying the 12- and 24-month SPI, starting from the mid-20th century. Similarly, the region of Damascus presented a similar pattern to those in Beirut, Amman, and Jerusalem. An upward trend in the frequency of extreme drought events was observed for the last thirty years. The same trend seems to be true in terms of the duration of dry periods. Drought events have also been observed in the central, southern, and eastern regions of Turkey. A downward trend was observed in Cairo based on a trend analysis of its monthly precipitation.
... In Euro-Mediterranean (climate change "hotspot" basin), increasing temperature trend and decreasing rainy days and precipitation deficit cause drought conditions with increasing frequency. Therefore, characterization of drought patterns in this basin are studied in detail by using index values of Palmer Drought Severity Index (PDSI; Briffa et al., 1994;Mika et al., 2005;Trnka et al., 2016;Vasiliades & Loukas, 2009;Vicente-Serrano et al., 2015), Standardized Precipitation Index (SPI; Br azdil et al., 2016;Oikonomou et al., 2020;Trnka et al., 2016;Vicente-Serrano et al., 2021;Vido & Nalevankov a, 2020), Standardized Precipitation Evapotranspiration Index (SPEI; Li et al., 2015;Manzano et al., 2019;Vicente-Serrano et al., 2010). For Europe, the impacts of drought on agriculture (Gil et al., 2011;Hlavinka et al., 2009;Jayanthi et al., 2014;Potop, 2011;Quijano et al., 2015), surface water resources (Vicente-Serrano et al., 2014), forestry (Muukkonen et al., 2015;Vicente-Serrano et al., 2012), human mortality (Dilley et al., 2005) and energy and industry (Stagge et al., 2015) are generally investigated in detail. ...
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As a natural disaster, drought affects many sectors such as agriculture and hydrology, as well as having an effect on air quality. In terms of air pollution, drought can reduce wet scavenging of pollutants and change their chemical production/loss and lifetime. This study investigates the relationship between drought events and air pollutants in Turkey. As a drought indicator, the Standardized Precipitation‐Evapotranspiration Index (SPEI)‐1 monthly values for dry (SPEI < −0.99), normal (−0.99 < SPEI < 0.99) and wet (SPEI < 0.99) conditions were used to investigate the changes in PM 10 , PM 2.5 , O 3 concentration levels. Monthly mean PM 10 values of 80 stations for the period 2010–2018, PM 2.5 and O 3 values of 10 and 12 stations, respectively, were used for the analysis throughout the 2014–2018 period. According to the results, while frequency occurrence of normal conditions decreased in the last period (2010–2018) when compared to the first (1901–2009), drought conditions have significantly increased in each region of Turkey in the last decade. Highest increase in drought events occurred in the inner/southern parts of Turkey. In dry events, while PM 10 levels of the stations show above‐normal values, highest regional increase in PM 10 was found in the Central Anatolia (CAR), Mediterranean (MeR), Aegean (AR) and Marmara (MR) regions of the country. In fall, high daily temperatures and cloudless days in CAR and MeR regions are seen under deep surface low over continental Europe and surface high over Caspian Sea, which result in severe dryness events and associated high PM 10 values in the air quality stations. On the other hand, as a consequence of the expanding Asiatic monsoon low to the eastern part of Turkey, significant amount of moisture is transferred from the Eastern Mediterranean Sea surface to the CAR and MeR regions by southerly flows (wetness SPEI conditions in fall) and cause to appear below‐normal PM 10 values in the southern stations.
... There are studies that suggest an increasing trend (e.g., Dai, 2011Dai, , 2013Sheffield et al., 2012;Trnka et al., 2016), a decreasing trend (e.g., Spinoni et al., 2014) and no trend (e.g., Spinoni et al., 2019;Oikonomou et al., 2020;Vicente-Serrano et al., 2021) for droughts for the past decades in the central European region. The discrepancies in the findings are due to the complex characteristics and several different ways of defining (Mishra and Singh, 2010;D. ...
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Droughts are among the most relevant natural disasters related to climate change. We evaluated different regional climate model outputs and their ability to reproduce observed drought indices in Germany and its near surroundings between 1980–2009. Both outputs of an ensemble of six EURO-CORDEX models of 12.5 km grid resolution and outputs from a high-resolution (5 km) Weather Research and Forecasting (WRF) run were employed. The latter model was especially tailored for the study region regarding the physics configuration. We investigated drought-related variables and derived the 3-month standardized precipitation evapotranspiration index (SPEI-3) to account for meteorological droughts. Based on that, we analyzed correlations, the 2003 event, trends and drought characteristics (frequency, duration and severity) and compared the results to E-OBS. Methods used include Taylor diagrams, the Mann–Kendall trend test and the spatial efficiency (SPAEF) metric to account for spatial agreement of patterns. Averaged over the domain, meteorological droughts were found to occur approximately 16 times in the study period with an average duration of 3.1 months and average severity of 1.47 SPEI units. WRF's resolution and setup were shown to be less important for the reproduction of the single drought event and overall drought characteristics. Depending on the specific goals of drought analyses, computation resources could therefore be saved, since a coarser resolution can provide similar results. Benefits of WRF were found in the correlation analysis. The greatest benefits were identified in the trend analysis: only WRF was able to reproduce the observed negative SPEI trends to a fairly high spatial accuracy, while the other regional climate models (RCMs) completely failed in this regard. This was mainly due to the WRF model settings, highlighting the importance of appropriate model configuration tailored to the target region. Our findings are especially relevant in the context of climate change studies, where the appropriate reproduction of trends is of high importance.
... Flash droughts (FDs) are a special form of drought. In contrast to the descriptions of classical droughts (de Araújo & Bronstert 2015;Oikonomou et al. 2020), FDs are characterised by rapid onset and relatively short durations (Otkin et al. 2018;Lisonbee et al. 2021). They are associated with severe and immediate soil moisture depletions, resulting in plant water stress and mortality (Ford & Labosier 2017;Liang & Yuan 2021;Osman et al. 2021). ...
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Many definitions and delineation methods exist for identifying flash droughts (FDs), which are events of rapid and unusual large depletion of root-zone soil moisture, in comparison to average moisture conditions, due to climatic compound conditions over a short period of several weeks. Six FD identification methods were compared to analyse their functioning using data from several experimental cropland sites across Central Europe. Co- and misidentification of the FD time series were assessed using confusion and synchronicity metrics on a local scale. Even though a large degree of synchronicity of individual FD events was observed, some divergence in drought periods was detected, which was related to four intrinsic differences in the underlying FD definitions: (1) type of critical variable; (2) velocity of drought intensification; (3) pre-set threshold values for final depletion and/or (4) minimum length of the duration of FDs. To balance the strengths and weaknesses of those methods that are not based on soil moisture, we suggest using an ensemble approach for event identification, which is validated in this study for the temperate central European region. In doing so, the current unclearly defined sub-types of FDs can be detected, regardless of the different combinations of compound drivers and differences in intensification dynamics. All methods were implemented in an R package and are available as a Shiny app for the public. HIGHLIGHTS The multiple methods proposed to identify flash droughts (FDs) show substantial disagreement.; Soil moisture is the key variable to identify FDs in croplands; however, such data are scarce, and a method based on proxy variables is necessary.; A multi-index or multi-method should be favoured in identifying FDs, as a single proxy (to soil moisture) may cause significant misidentification.;