Geological records indicate only a modest Last Glacial Maximum (LGM) increase in dust deposition over the Third Pole (TP), in contrast to the order‐of‐magnitude rise at high latitudes. Existing climate simulations, which generally prescribe present‐day or no TP glaciers, have struggled to reproduce this muted response....
Qiang Wei, Miao Wang, Zheng-Guo Shi et al.· Geophysical Research Letters· 0 citations
Deep-time hyperthermal/transient warming events provide critical analogs for modern climatic warming and its impacts. However, all ancient hyperthermals documented to date have occurred under greenhouse climate states, limiting their relevance for understanding the trajectory of present-day climate change. Here, we pre...
L. Yao, Thomas J. Algeo, Qiu-Lai Wang et al.· Proceedings of the National...· 0 citations
The Late Ordovician marks the first major continental ice sheet event in the Phanerozoic Eon, despite high CO
2
levels, coinciding with a dramatic global temperature drop and one of the largest mass extinctions. However, the critical role of ice sheet-climate feedbacks in driving the Late Ordovician glaciation rema...
Yu-Dong Sun, Yong-Gang Liu, Jia-Cheng Wu et al.· Climate of the Past· 0 citations
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