In the Akmola region, recent studies on potential evapotranspiration from 1991 to 2021 showed a decreasing trend, ranging between 632mm and 850mm, with no significant change observed, particularly in the BNNP area [ 58 ].
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Unravelling long-term impact of water abstraction and climate change on endorheic lakes: A case study of Shortandy Lake in Central Asia.
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