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A southern and northern control on speleothem-based Asian summer monsoon variability during MIS 4

Published online by Cambridge University Press:  09 July 2019

Dianbing Liu Open the ORCID record for Dianbing Liu [Opens in a new window] ,
Shushuang Liu  and
Yifan Fang
Dianbing Liu*
Affiliation:
School of Geography, Nanjing Normal University, Nanjing 210023, China
Shushuang Liu
Affiliation:
School of Geography, Nanjing Normal University, Nanjing 210023, China
Yifan Fang
Affiliation:
School of Geography, Nanjing Normal University, Nanjing 210023, China
*
*Corresponding author at: School of Geography, Nanjing Normal University, Nanjing 210023, China. E-mail address: ldb9921@njnu.edu.cn (D.B. Liu).
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Abstract

A 20-year-resolution speleothem δ18O record from southern China reveals a detailed Asian summer monsoon (ASM) history between 73.6 and 62.3 ka. ASM changes during Interstadial 19 and late MIS 4 matched Greenland temperature variations but were antiphased with Antarctic temperatures. However, long-term strengthening of the ASM in early MIS 4 agrees well with the gradual Antarctic warming, when Greenland remained in a stable cold state. More specifically, the ASM was less variable during peak interstadials in contrast to striking instabilities during stadials. These observations suggest that the factors dominating ASM variability change through time. During early MIS 4, negligible freshwater perturbations occurred in the North Atlantic, and sea-surface temperatures in the low- to midlatitude Pacific Ocean reached the modern level. Thus, an expansion of the Intertropical Convergence Zone (ITCZ) was likely important for the long-term ASM rise. In late MIS 4, the antiphase correlation between ASM and Antarctic temperature could be attributed to freshwater inputs into the North Atlantic and a southerly positioned ITCZ. Consequently, meridional ITCZ shifts, although within a limited latitudinal band, would result in an antiphase relationship between interhemispheric climate changes. Otherwise, an in-phase correlation could be expected if the centroid of ITCZ is stable along the equator.

Keywords

Speleothem recordASM variabilityMIS 4Interhemispheric climate correlationExpansion/contraction of ITCZ
Type
Research Article
Information
Quaternary Research , Volume 92 , Issue 3 , November 2019 , pp. 738 - 753
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2019 

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