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Central Asian rivers under climate change: Impacts assessment in eight representative catchments

Iulii DidovetsPotsdam Institute for Climate Impact Research, Telegraphenberg A 31, 14473, Potsdam, GermanyAnastasia LobanovaPotsdam Institute for Climate Impact Research, Telegraphenberg A 31, 14473, Potsdam, GermanyValentina KrysanovaPotsdam Institute for Climate Impact Research, Telegraphenberg A 31, 14473, Potsdam, GermanyChristoph MenzPotsdam Institute for Climate Impact Research, Telegraphenberg A 31, 14473, Potsdam, GermanyZhanna BabagalievaThe Regional Environmental Centre for Central Asia, Orbita 1, Almaty, KazakhstanAliya NurbatsinaNadejda GavrilenkoCentre of Hydrometeorological Service of the Republic of Uzbekistan, 72, 1st Bodomzor Yuli Str., Tashkent, 100052, UzbekistanVohid KhamidovAtabek UmirbekovLeibniz Institute of Agricultural Development in Transition Economies, Theodor-Lieser-Str. 2, 06120, Halle, GermanySobir QodirovTashkent Institute of Engineers of Irrigation and Mechanization of Agriculture, 39 Kari Niyazov Street, Tashkent, 100000, UzbekistanDowletgeldi MuhyyewHydrometeorology Service of the Ministry of Agriculture and Environmental Protection of the Turkmenistan, Oguzkhan Ave. 203, Ashgabat, 744028, TurkmenistanFred F. HattermannPotsdam Institute for Climate Impact Research, Telegraphenberg A 31, 14473, Potsdam, Germany
ABI

Аннотация

Eight river catchments within Central Asia. The limited amount of water resources is already an issue in the Central Asian region, and climate change may be crucial for water availability and development of countries in the region. This study investigates potential climate change impacts on water resources in Central Asia to the end of the century by focusing on eight river catchments with diverse natural conditions located in different countries. The eco-hydrological model SWIM was setup, calibrated and validated for all selected catchments under study. Scenarios from five bias-corrected GCMs under Representative Concentration Pathways 4.5 and 8.5 were used to drive the hydrological model. The results show an increase of mean annual temperature in all catchments for both RCPs to the end of the century. The projected changes in annual precipitation indicate a clear trend to increase in the Zhabay and to decrease in the Murghab catchments, and for other catchments, they were smaller. The projected trends for river discharge are similar to those of precipitation, with an increase in the north and decrease in the south of the study region. Seasonal changes are characterized by a shift in the peak of river discharge up to one month, shortage of snow accumulation period, and reduction of discharge in summer months.

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