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pro vyhledávání: '"Siya ZOU"'
Publikováno v:
地质科技通报, Vol 43, Iss 1, Pp 173-183 (2024)
Objective The Holocene climate of the Tibetan Plateau (TP) is mainly controlled by midlatitude westerlies, the East Asian monsoon, and the Indian monsoon. Previous studies have identified different patterns of Holocene climate change in different reg
Externí odkaz:
https://doaj.org/article/a4eed0aa9f7c434db7ee3c4a5fdc12e1