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A 550,000-year record of East Asian monsoon rainfall from 10Be in loess

TLDR
A 550,000-year-long record of East Asian summer monsoon rainfall from Chinese loess is derived, arguing that both EASM intensity and Chinese cave δ18O are not governed by high-northern-latitude insolation, as suggested by others, but rather by low-latitudes interhemispheric insolation gradients, which may also strongly influence global ice volume via monsoon dynamics.
Abstract
Cosmogenic 10 Be flux from the atmosphere is a proxy for rainfall. Using this proxy, we derived a 550,000-year-long record of East Asian summer monsoon (EASM) rainfall from Chinese loess. This record is forced at orbital precession frequencies, with higher rainfall observed during Northern Hemisphere summer insolation maxima, although this response is damped during cold interstadials. The 10 Be monsoon rainfall proxy is also highly correlated with global ice-volume variations, which differs from Chinese cave δ 18 O, which is only weakly correlated. We argue that both EASM intensity and Chinese cave δ 18 O are not governed by high-northern-latitude insolation, as suggested by others, but rather by low-latitude interhemispheric insolation gradients, which may also strongly influence global ice volume via monsoon dynamics.

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Precession-band variance missing from East Asian monsoon runoff

TL;DR: A record of local precipitation and runoff from the East Chain Sea is presented, which indicates strong sensitivity to greenhouse gases and high latitude ice sheet forcing and suggests that East Asian monsoon rainfall is more sensitive to greenhouse gas and high-latitude ice sheetforcing than to direct insolation forcing.
Journal ArticleDOI

New insights on Chinese cave δ18O records and their paleoclimatic significance

TL;DR: Wang et al. as discussed by the authors provided new insights into Chinese cave δ18O records and their paleoclimatic significance, based on recent research progress, and showed that Chinese cave records do not reflect changes in summer rainfall throughout the whole of eastern monsoonal China, which is evident by comparing monitored summer rainfall amount in eastern China and an integrated Chinese cave Δ18Osyn proxy.
References
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Journal ArticleDOI

The NCEP/NCAR 40-Year Reanalysis Project

TL;DR: The NCEP/NCAR 40-yr reanalysis uses a frozen state-of-the-art global data assimilation system and a database as complete as possible, except that the horizontal resolution is T62 (about 210 km) as discussed by the authors.
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A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records

TL;DR: In this paper, a 53-Myr stack (LR04) of benthic δ18O records from 57 globally distributed sites aligned by an automated graphic correlation algorithm is presented.
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Some simple solutions for heat-induced tropical circulation.

TL;DR: In this article, a simple analytic model is constructed to elucidate some basic features of the response of the tropical atmosphere to diabatic heating, showing that there is considerable east-west asymmetry which can be illustrated by solutions for heating concentrated in an area of finite extent.
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Insolation values for the climate of the last 10 million years

TL;DR: In this article, new values for the astronomical parameters of the Earth's orbit and rotation (eccentricity, obliquity and precession) are proposed for paleoclimatic research related to the Late Miocene, the Pliocene and the Quaternary.
Journal ArticleDOI

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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