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- W4386157657 abstract "Striking changes in Asian palaeohydrology occurred during the late Quaternary. Our knowledge has recently been enhanced by new studies, including an update of the Late Quaternary Chinese Lake Data Base and the comparison of multiple lake-level records with paleoclimate simulations. In the Middle East and Tibetan Plateau regions, lake levels declined overall from 30,000 a BP to present. Low lake levels and inferred aridity in central and eastern Asia during the LGM likely reflect a weakened summer monsoon. With mid-Holocene, insolation-driven enhancement of the monsoon, lake levels increased from Arabia to northeast China, although other circulation adjustments caused lower levels northwest and southeast of the monsoon belt." @default.
- W4386157657 created "2023-08-26" @default.
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- W4386157657 date "2023-01-01" @default.
- W4386157657 modified "2023-09-25" @default.
- W4386157657 title "Lake level studies | Asia" @default.
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- W4386157657 doi "https://doi.org/10.1016/b978-0-323-99931-1.00074-x" @default.
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