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青藏高原“大湖期”的時(shí)空復(fù)雜性(英文)

發(fā)布時(shí)間:2022-02-11 19:20
  <正>As the "Asian Water Tower" and the source of many major rivers in Asia,the Tibetan Plateau(TP) significantly affects human societies in densely-populated Asia [1].Lakes in the TP have a total area of ~5 × 104 km2 and hence they comprise an important component of the "Asian Water Tower". These lakes are sensitive to climate changes and have exhibited an overall trend of rapid expansion during recent decades[2].Well-preserved shorelines 

【文章來源】:Science Bulletin. 2020,65(16)EISCICSCD

【文章頁數(shù)】:3 頁

【參考文獻(xiàn)】:
期刊論文
[1]Strengthened Indian summer monsoon brought more rainfall to the western Tibetan Plateau during the early Holocene[J]. Xiangjun Liu,Xiaojian Zhang,Yanluan Lin,Liya Jin,Fahu Chen.  Science Bulletin. 2019(20)
[2]A robust but variable lake expansion on the Tibetan Plateau[J]. Guoqing Zhang,Wei Luo,Wenfeng Chen,Guoxiong Zheng.  Science Bulletin. 2019(18)
[3]Underestimated 14C-based chronology of late Pleistocene high lake-level events over the Tibetan Plateau and adjacent areas: Evidence from the Qaidam Basin and Tengger Desert[J]. LONG Hao,SHEN Ji.  Science China(Earth Sciences). 2015(02)



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