State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Gilles Ramstein
Laboratoire des Sciences du Climat et de l’Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
Lin Ding
State Key Laboratory of Tibetan Plateau Earth System, Environment and Resources (TPESER), Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China
Tianjun Zhou
LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
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EndNote: 147
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Total article views: 1,615 (including HTML, PDF, and XML)
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1,233
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1,615
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PDF: 314
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BibTeX: 76
EndNote: 102
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Total article views: 1,045 (including HTML, PDF, and XML)
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487
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Total: 1,045
Supplement: 160
BibTeX: 39
EndNote: 45
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Viewed (geographical distribution)
Total article views: 2,660 (including HTML, PDF, and XML)
Thereof 2,660 with geography defined
and 0 with unknown origin.
Total article views: 1,615 (including HTML, PDF, and XML)
Thereof 1,615 with geography defined
and 0 with unknown origin.
Total article views: 1,045 (including HTML, PDF, and XML)
Thereof 1,045 with geography defined
and 0 with unknown origin.
Our research explores the intensification of the South Asian summer monsoon (SASM) during the Middle Miocene (17–12 Ma). Using an advanced model, we reveal that the uplift of the Iranian Plateau significantly influenced the SASM, especially in northwestern India. This finding surpasses the impact of factors like Himalayan uplift and global CO2 changes. We shed light on the complex dynamics shaping ancient monsoons, providing valuable insights into Earth's climatic history.
Our research explores the intensification of the South Asian summer monsoon (SASM) during the...
