Westerlies Asia and monsoonal Asia: Spatiotemporal differences in climate change and possible mechanisms on decadal to sub-orbital timescales
The 'westerlies-dominated climatic regime'(WDCR) in the present interglacial period was
proposed because precipitation/moisture variations between arid central Asia and mid …
proposed because precipitation/moisture variations between arid central Asia and mid …
Hydroclimatic changes in China and surroundings during the Medieval Climate Anomaly and Little Ice Age: spatial patterns and possible mechanisms
Investigating hydroclimatic changes during key periods such as the Medieval Climate
Anomaly (MCA, 1000–1300 AD) and the Little Ice Age (LIA, 1400–1900 AD) is of …
Anomaly (MCA, 1000–1300 AD) and the Little Ice Age (LIA, 1400–1900 AD) is of …
The Indian monsoon variability and civilization changes in the Indian subcontinent
The vast Indo-Gangetic Plain in South Asia has been home to some of the world's oldest
civilizations, whose fortunes ebbed and flowed with time—plausibly driven in part by shifts in …
civilizations, whose fortunes ebbed and flowed with time—plausibly driven in part by shifts in …
Holocene East Asian summer monsoon records in northern China and their inconsistency with Chinese stalagmite δ18O records
Monsoon precipitation over China exhibits large spatial differences. It has been found that a
significantly enhanced East Asian summer monsoon (EASM) is characterized by increased …
significantly enhanced East Asian summer monsoon (EASM) is characterized by increased …
A review on the Indian summer monsoon rainfall, variability and its association with ENSO and IOD
PH Hrudya, H Varikoden, R Vishnu - Meteorology and Atmospheric …, 2021 - Springer
The Indian summer monsoon rainfall (ISMR) during June to September contributes most of
the annual rainfall over India and plays an important role in Indian agriculture and thus the …
the annual rainfall over India and plays an important role in Indian agriculture and thus the …
Circulation effect: response of precipitation δ18O to the ENSO cycle in monsoon regions of China
M Tan - Climate Dynamics, 2014 - Springer
Inter-annual variation in the ratio of 18 O to 16 O of precipitation (δ 18 O p) in the monsoon
regions of China (MRC, area approximately east of 100° E) has not yet been fully analyzed …
regions of China (MRC, area approximately east of 100° E) has not yet been fully analyzed …
Main controls on the stable carbon isotope composition of speleothems
J Fohlmeister, NRG Voarintsoa, FA Lechleitner… - … et Cosmochimica Acta, 2020 - Elsevier
The climatic controls on the stable carbon isotopic composition (δ 13 C) of speleothem
carbonate are less often discussed in the scientific literature in contrast to the frequently …
carbonate are less often discussed in the scientific literature in contrast to the frequently …
An abrupt shift in the Indian monsoon 4000 years ago
Indian Summer Monsoon (ISM) precipitation during the twentieth century is characterized by
a biennial oscillation, such that ISM precipitation varied between singularly strong and weak …
a biennial oscillation, such that ISM precipitation varied between singularly strong and weak …
Trends and oscillations in the Indian summer monsoon rainfall over the last two millennia
Observations show that summer rainfall over large parts of South Asia has declined over the
past five to six decades. It remains unclear, however, whether this trend is due to natural …
past five to six decades. It remains unclear, however, whether this trend is due to natural …
[HTML][HTML] 高分辨率石笋记录的近700 年来滇西南夏季风降水变化
陈越， 王欢， 刘宏， 王芳， 李苗发， 程海， 马志邦… - 第四纪研究, 2021 - html.rhhz.net
基于云南西南部司岗里洞一支长约168 mm 石笋(编号SGL1) 的7 个230 Th 年龄和325 个δ 18 O
数据, 建立了1322~ 1605 AD 和1700~ 1927 AD 时段平均分辨率达2 a 的夏季风降水演化序列 …
数据, 建立了1322~ 1605 AD 和1700~ 1927 AD 时段平均分辨率达2 a 的夏季风降水演化序列 …