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Jiangying Wu

Researcher at Nanjing Normal University

Publications -  32
Citations -  5527

Jiangying Wu is an academic researcher from Nanjing Normal University. The author has contributed to research in topics: Computer science & East Asian Monsoon. The author has an hindex of 10, co-authored 13 publications receiving 4879 citations. Previous affiliations of Jiangying Wu include Nanjing University & University of Minnesota.

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A High-Resolution Absolute-Dated Late Pleistocene Monsoon Record from Hulu Cave, China

TL;DR: The record links North Atlantic climate with the meridional transport of heat and moisture from the warmest part of the ocean where the summer East Asian Monsoon originates and generally agrees with the timing of temperature changes from the Greenland Ice Sheet Project Two (GISP2).
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The holocene Asian monsoon : links to solar changes and North Atlantic climate

TL;DR: A 5-year-resolution absolute-dated oxygen isotope record from Dongge Cave, southern China, provides a continuous history of the Asian monsoon over the past 9000 years, and shows that some, but not all, of the monsoon variability at these frequencies results from changes in solar output.
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A high-resolution stalagmite record of the Holocene East Asian monsoon from Mt Shennongjia, central China

TL;DR: In this paper, high-resolution oxygen isotope (δ18O) profiles of six stalagmites from Sanbao Cave in Hubei province, central China, were used to provide a continuous history of East Asian Summer Monsoon (EASM) intensity for the period from 13-0.2 thousand years before present (ky BP, relative to AD 1950).
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Long-term trend and abrupt events of the Holocene Asian monsoon inferred from a stalagmite δ10O record from Shennongjia in Central China

TL;DR: In this paper, a high-resolution oxygen-isotope record from a thorium-uranium-dated stalagmite from Shanbao Cave at Shennongjia reflects variations in the amount of monsoon precipitation for the period from 11.5 to 2.1 ka (1 ka = 1000 cal aBP).
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A detailed comparison of Asian Monsoon intensity and Greenland temperature during the Allerød and Younger Dryas events

TL;DR: In this paper, an annual layer-counted and 230Th-dated stalagmite oxygen isotope record from Qingtian Cave in Hubei province, central China, provides an Asian Monsoon (AM) history across the Allerod to Younger Dryas (YD) transition, with an average 2.5-year resolution.