Abstract
Seasonal drought is often overlooked because its impacts are less devasting than meteorological or hydrological drought. Nevertheless, short-term drought can have significant impacts on soil moisture content, agricultural crop yield, and sand and dust storms. Using data obtained from bias-corrected regional climate modelling (RCM) outputs, future seasonal drought is investigated over the water-scarce Arab domain using SPI-3. The climate modelling outputs include three downscaled mainframe GCMs downscaled using a single RCM for two climate scenarios: RCP4.5 and RCP8.5. Results across the region exhibit spatial and temporal variability. For example, Rift Valley, in the eastern sub-Sahara, projects less frequent and less severe drought, particularly during the winter (DJF) months. Conversely, the Morocco Highlands and adjacent Mediterranean coast signals a dramatic increase in drought by end-century during winter (DJF) and spring (MAM). Moderate increase in drought indicated in the greater Mashreq in spring (MAM) can be linked to sand and dust storm risk. Thirdly, autumn drought (SON) is linked to increased forest fire risk in the Levant. Projected increases in drought frequency and severity call for adaptation measures to reduce impacts.
Highlights
United Nations Economic and Social Commission for Western Asia, Beirut 1107 2260, Lebanon; Abstract: Seasonal drought is often overlooked because its impacts are less devasting than meteorological or hydrological drought
Historical and projected drought was calculated based on the 3-month Standardized Precipitation Index (SPI) using precipitation obtained from bias-corrected regional climate modelling outputs
The mean change in the number of events based on RCP4.5 (Figure 2) and RCP8.5 (Figure 3) reveal projected seasonal drought variability
Summary
United Nations Economic and Social Commission for Western Asia, Beirut 1107 2260, Lebanon; Abstract: Seasonal drought is often overlooked because its impacts are less devasting than meteorological or hydrological drought. These events are less severe and shorter in duration compared to meteorological drought, they occur over twice as often [23].Trend analysis in the region has revealed an expected increase in Academic Editors: Corrado Camera and Georgios Zittis The region generally projects an increase >1.5 ◦ C by mid-century, compared to the recent reference period. By end-century, summer (JJA) trends disagree in the Senegal River (SR), but project a notable increase (up to 18%) during autumn (SON).
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