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
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
Orbital variations redistribute seasonal insolation and can reorganize tropical rainfall, atmospheric circulation, and high‐latitude surface conditions. The energetic linkage among these processes during the late Paleozoic Ice Age remains poorly constrained. We use a 21‐member fully coupled orbital ensemble generated w...
Ren Wei, Zhi-Jun Jin, Ming-Song Li et al.· Journal of Geophysical Resea...· 0 citations
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