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- W4214520121 abstract "降水再循环率(即蒸发-降水反馈强度)和水汽来源是区域水循环的两个关键环节, 它们的量化对于理解水循环过程及其变化至关重要. 关于青藏高原降水再循环率和水汽源的已有研究结果存在很大争议. 文章厘清了理解水循环的不同视角, 指出蒸发与降水之比主要取决于气候模态, 而降水再循环率还与区域大小密切相关, 水汽源区则取决于追踪时段(降水时段或非降水时段)和追踪程度. 在同一理论框架下, 关于青藏高原水循环的不同研究结果之间不存在根本冲突." @default.
- W4214520121 created "2022-03-02" @default.
- W4214520121 creator A5028911353 @default.
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- W4214520121 date "2021-12-17" @default.
- W4214520121 modified "2023-09-28" @default.
- W4214520121 title "青藏高原降水再循环率与水汽来源辨析" @default.
- W4214520121 doi "https://doi.org/10.1360/sste-2021-0255" @default.
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