The 4.2 ka event was a widespread abrupt cooling event in the Northern Hemisphere.
However, there was a spatially inconsistent hydroclimatic response to the 4.2 ka event in the …

Investigation of summer extreme precipitation during past warm periods may deepen our
understanding of its behavior in current and future warmer climates. In this study, we …

In parallel with pronounced cooling in the oceans, vast areas of the continents experienced
enhanced aridification and restructuring of vegetation and animal communities during the …

Land surface temperature (LST) is a key parameter in the study of surface energy balance
and climate change from local through to global scales. Vegetation has inevitably influenced …

In this study, we employ biological, geochemical and mineral, and physical proxies to
quantitatively and semi-quantitatively reconstruct regional paleoclimate variations in China …

The northern fringe area of the East Asian summer monsoon (EASM) between arid and
semiarid regions is a fragile eco-environment zone and ecological transition zone, and it is …

Pliocene warmth has been used as an analogue for predicting climate response to the rapid
atmospheric CO2 increase in the future. Pedogenic carbonates provide an essential archive …

Past intervals of warming provide the unique opportunity to observe how the East Asia
monsoon precipitation response happened in a warming world. However, the available …

The remote forcing from land surface changes in the Sahara is hypothesized to play a
pivotal role in modulating the intensity of the East Asian summer monsoon (EASM) through …

Abstract The Paleocene–Eocene Thermal Maximum (PETM,~ 56 Ma) was a geologically
abrupt and extreme global warming event that had a profound effect on global climate and …