New insights on Chinese cave δ18O records and their paleoclimatic significance
In the last two decades, stalagmite oxygen isotope (δ 18 O) records have been widely used
to study the evolution of the paleomonsoon. Nevertheless, interpreting cave δ 18 O records …
to study the evolution of the paleomonsoon. Nevertheless, interpreting cave δ 18 O records …
Holocene climatic optimum in the East Asian monsoon region of China defined by climatic stability
It is unclear whether the Holocene climatic optimum (HCO) occurred synchronously
throughout the East Asian summer monsoon (EASM) region, and if it did, whether it occurred …
throughout the East Asian summer monsoon (EASM) region, and if it did, whether it occurred …
Deciphering local and regional hydroclimate resolves contradicting evidence on the Asian monsoon evolution
The winter and summer monsoons in Southeast Asia are important but highly variable
sources of rainfall. Current understanding of the winter monsoon is limited by conflicting …
sources of rainfall. Current understanding of the winter monsoon is limited by conflicting …
Dipolar mode of precipitation changes between north China and the Yangtze River Valley existed over the entire Holocene: Evidence from the sediment record of …
Instrumental data indicate the occurrence of a dipolar pattern of precipitation anomalies
between north China and the Yangtze River Valley (YRV), which was termed “northern …
between north China and the Yangtze River Valley (YRV), which was termed “northern …
Investigating the long-term palaeoclimatic controls on the δD and δ18O of precipitation during the Holocene in the Indian and East Asian monsoonal regions
Z Rao, Y Li, J Zhang, G Jia, F Chen - Earth-Science Reviews, 2016 - Elsevier
This paper aims to achieve an improved understanding of the long-term change trends of
precipitation δD and δ 18 O values (δD p and δ 18 O p) in the Asian monsoonal region and …
precipitation δD and δ 18 O values (δD p and δ 18 O p) in the Asian monsoonal region and …
A 13,000-year peatland palaeohydrological response to the ENSO-related Asian monsoon precipitation changes in the middle Yangtze Valley
Quantitative reconstructions of the depth to water table (DWT) of ombrotrophic (rain-fed)
peatlands are important for understanding the palaeohydrological responses of peatlands to …
peatlands are important for understanding the palaeohydrological responses of peatlands to …
Millennial-scale Asian summer monsoon variations in South China since the last deglaciation
X Wang, G Chu, M Sheng, S Zhang, J Li, Y Chen… - Earth and Planetary …, 2016 - Elsevier
Characterizing spatiotemporal variability of the Asian summer monsoon (ASM) is critical for
full understanding of its behavior, dynamics, and future impacts. The present knowledge …
full understanding of its behavior, dynamics, and future impacts. The present knowledge …
On the timing of the East Asian summer monsoon maximum during the Holocene—Does the speleothem oxygen isotope record reflect monsoon rainfall variability?
The evolution of the East Asian summer monsoon (EASM) during the Holocene has long
been of significant interest. Knowledge of past EASM variability not only increases our …
been of significant interest. Knowledge of past EASM variability not only increases our …
[PDF][PDF] 全新世东亚夏季风最强盛期出现在何时?——兼论中国南方石笋氧同位素的古气候意义
陈建徽， 饶志国， 刘建宝， 黄伟， 董广辉， 胡玉… - 中国科学: 地球 …, 2016 - researchgate.net
摘要探寻全新世东亚夏季风演变过程, 不仅有利于在更长时间尺度上深化对季风动力学的理解,
也能够为研究中华文明发展提供环境和气候背景, 因此历来受到研究者的重视. 然而 …
也能够为研究中华文明发展提供环境和气候背景, 因此历来受到研究者的重视. 然而 …
[HTML][HTML] Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation …
Abstract The East Asian summer monsoon (EASM) northern boundary is a critical indicator
of EASM variations. Movement of the boundary is modulated by both the EASM and the mid …
of EASM variations. Movement of the boundary is modulated by both the EASM and the mid …