Assessment of climate change in Central Asia from 1980 to 2100 using the Koppen-Geiger climate classification

The accelerated global warming and heterogeneous change in precipitation have been resulting in climate system shifts, which plays a key role in the stability of ecosystem and social economic development. Central Asia is account 80% of the temperate desert, characterized by fragile ecosystem; howeve...

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Bibliographic Details
Published in:Atmosphere
Main Authors: He, Huili, Luo, Geping, Cai, Peng, Hamdi, Rafiq, Termonia, Piet, De Maeyer, Philippe, Kurban, Alishir, Li, Jianjun
Format: Article in Journal/Newspaper
Language:English
Published: 2021
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Online Access:https://biblio.ugent.be/publication/8694642
http://hdl.handle.net/1854/LU-8694642
https://doi.org/10.3390/atmos12010123
https://biblio.ugent.be/publication/8694642/file/8694645
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Summary:The accelerated global warming and heterogeneous change in precipitation have been resulting in climate system shifts, which plays a key role in the stability of ecosystem and social economic development. Central Asia is account 80% of the temperate desert, characterized by fragile ecosystem; however, it has experienced the fastest warming in recent decades and projected warming in future. The Koppen-Geiger climate classification is a useful tool to assess the potential impacts of climate change on regional ecosystem. The spatial shift and temporal evolution of each climatic zone based on Koppen-Geiger climate classification are analyzed in historical and future period under different scenarios (RCP2.6, RCP4.5 and RCP8.5), high risk regions that might experience more frequent climatic zone shifts are delimited in this study, which could provide the useful information for developing mitigate strategies in coping with the warming threat. The hotter and dryer subtypes of arid climatic zone and warmer subtypes of temperate climatic zone expanded their coverage in Central Asia, corresponding to the tundra climatic, cooler subtype of arid and temperate climatic zone contracted. Based on a method defining the climate-sensitivity, high risk regions are mainly distributed in northern Kazakhstan and Tianshan Mountains region.