This paper reviews recent advances regarding land–atmosphere–ocean coupling
associated with the Tibetan Plateau (TP) and its climatic impacts. Thermal forcing over the …

While the Atlantic Ocean is ventilated by high-latitude deep water formation and exhibits a
pole-to-pole overturning circulation, the Pacific Ocean does not. This asymmetric global …

Abstract The most recent Intergovernmental Panel on Climate Change assessment report
concludes that the Atlantic Meridional Overturning Circulation (AMOC) could weaken …

The meridional overturning circulation (MOC) in the ocean is a key player in the global
climate system, while continental topography provides an essential backdrop to the system …

Assessing the impact of future anthropogenic carbon emissions is currently impeded by
uncertainties in our knowledge of equilibrium climate sensitivity to atmospheric carbon …

The dynamic and thermal effects of the Tibetan Plateau (TP) on the precipitation in the Asian
arid and monsoon regions were investigated using three numerical experiments—one using …

Numerical models are important tools for understanding the processes and feedbacks in the
Earth system, including those involving changes in atmospheric CO 2 (CO 2, atm) …

The reason for the initial rise in atmospheric CO 2 during the last deglaciation remains
unknown. Most recent hypotheses invoke Southern Hemisphere processes such as shifts in …

Glacial periods exhibit abrupt Dansgaard‐Oeschger (DO) climatic oscillations that are
thought to be linked to instabilities in the Atlantic meridional overturning circulation (AMOC) …

Geological data for the Early Eocene (56–47.8 Ma) indicate extensive global warming, with
very warm temperatures at both poles. However, despite numerous attempts to simulate this …