The evolution of the East Asian Summer Monsoon (EASM) and its mechanism since the
Holocene remains controversial. Here, we investigate four eolian sediment sequences in the …

Climatic and environmental changes in the northeastern Tibetan Plateau are controlled by
the Asian summer monsoon (ASM) and the westerlies, two key circulation components of the …

Previous palaeoclimatic studies in the northeastern Qinghai-Tibetan Plateau (NETP) during
the Holocene, mainly using lake sediments, have deepened our understanding of the …

Abstract The northeastern Qinghai‐Tibetan Plateau (QTP) of China is located at the triple
junction of the Asian winter and summer monsoons and the westerlies, where paleoclimatic …

Lake Qinghai, located on the northeastern Tibetan Plateau north of the modern maximum
summer monsoon extent, is well situated to record northward advances of the summer …

Abstract The nature of Holocene Asian summer monsoon (ASM) evolution documented by
diverse natural archives remains controversial, with a contentious issue being whether or …

The variability and interaction of the East Asian summer monsoon (EASM) and mid-latitude
Westerlies have dominated Eurasian hydroclimates over orbital timescales and currently …

The pattern of changes in Holocene moisture conditions in the southern Tibetan Plateau
(TP) and the associated driving mechanism are still controversial. Here, we present the …

The moisture and precipitation evolution of mid-latitude Asia are dominated by the East
Asian summer monsoon (EASM) and mid-latitude Westerlies atmospheric systems. How …

Instrumental data suggest changes in the intensity of the East Asian Monsoon system over
the past century, possibly in response to anthropogenic climate change. To understand …