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Open access Sep 2026

Accelerated old basal ice loss in Tibetan glaciers after the 1990s

Surface meltwater that penetrates glacier interiors to the beds can warm the ice and enhance basal mass loss, exerting critical control over glacier dynamics. However, these processes remain poorly constrained in Tibetan Plateau glaciers, particularly those in the western sector, which have long been regarded as cold...

Bai-Qing Xu, Xiao-Long Zhang, T. Yao et al. · 0 citations
Open access Aug 2026

Glacier‐Climate Feedbacks Modulate Last Glacial Maximum Dust Cycle Over the Third Pole

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. · 0 citations

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