Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Wangting Ye
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Simin Peng
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Yuxin Zhang
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Hebin Liu
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Yichan Li
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Qin Han
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
Lingmei Xu
Key Laboratory of Western China's Environmental Systems (Ministry of
Education), College of Earth and Environmental Sciences, Center for
Hydrologic Cycle and Water Resources in Arid Region, Lanzhou University,
Lanzhou 730000, China
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Total article views: 1,969 (including HTML, PDF, and XML)
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Many closed-basin lakes are now drying, causing water crisis in hinterlands; however, many were much wetter in a similar warm world 6000 years ago. Why do they respond differently and will it be wetter or drier? We assess the wet–dry status and mechanism at different timescales and suggest that moisture change in the past and future warm periods are controlled by summer and winter precipitation, respectively. Diversified responses in different closed basins need a more resilient strategy.
Many closed-basin lakes are now drying, causing water crisis in hinterlands; however, many were...
