Aeolian activity on the Tibetan Plateau (TP) has profound effect on the Asian and global
climate. In the southern TP, loess deposition widely occurred associated with the massive …

High-latitude pelagic marine ecosystems are vulnerable to climate change because of the
intertwining of sea/continental ice dynamics, physics, biogeochemistry, and food-web …

Despite extensive investigation, the nature and causes of the Mid-Pleistocene Transition
remain enigmatic. In this work, we assess its linkage to asynchronous development of …

Distinguishing the independent contributions of tectonic denudation and climate‐driven
erosion on the production and supply of clastic materials of Chinese eolian deposits is …

High‐resolution records from past interglacial climates help constrain future responses to
global warming, yet are rare. Here, we produce seasonally resolved climate records from …

Proxy reconstructions suggest that increasing global mean sea surface temperature
(GMSST) during the last deglaciation was accompanied by a comparable or greater …

Multiple ice age cycles spanning the last three million years have fundamentally transformed
the Arctic landscape. The cadence, intensity and pattern of this glacial modification underpin …

Under sustained global warming, Arctic climate is projected to become more responsive to
changes in North Pacific meridional heat transport as a result of teleconnections between …

Pronounced model-observation discrepancies in the changes of tropical Pacific zonal sea
surface temperature gradient during the satellite era imply systematic model deficiencies …

The mid-Pleistocene transition (MPT)[~ 1.25 to 0.85 million years ago (Ma)] marks a shift in
the character of glacial-interglacial climate (,). One prevailing hypothesis for the origin of the …