On the glacial-interglacial variability of the Asian monsoon in speleothem δ 18 O records-Reference-Cited by-同舟云学术

On the glacial-interglacial variability of the Asian monsoon in speleothem δ 18 O records

Published:2020-02-14 Issue:7 Volume:6 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Liu G.¹²³^ORCID,Li X.⁴,Chiang H.-W.²^ORCID,Cheng H.⁴,Yuan S.¹²³^ORCID,Chawchai S.⁵^ORCID,He S.²^ORCID,Lu Y.²,Aung L. T.²⁶,Maung P. M.²⁷,Tun W. N.⁶^ORCID,Oo K. M.⁷,Wang X.²³^ORCID

Affiliation:

1. Interdisciplinary Graduate School, Nanyang Technological University, 639798 Singapore.

2. Earth Observatory of Singapore, Nanyang Technological University, 639798 Singapore.

3. Asian School of the Environment, Nanyang Technological University, 639798 Singapore.

4. Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an 710049, China.

5. Department of Geology, Chulalongkorn University, Bangkok 10330, Thailand.

6. Myanmar Earthquake Committee, Yangon 11052, Myanmar.

7. Department of Meteorology and Hydrology, Nay Pyi Taw 15011, Myanmar.

Abstract

Moisture transport pathway effect offsets glacial forcings, likely explaining a lack of G-IG variability in Chinese cave records.

Funder

National Research Foundation-Prime Minister's office, Republic of Singapore

National Natural Science Foundation of China

Development and Promotion of Science and Technology Talents Project

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference91 articles.

1. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years

2. The Asian monsoon over the past 640,000 years and ice age terminations

3. Global Monsoon Dynamics and Climate Change

4. Orbital-scale timing and mechanisms driving Late Pleistocene Indo-Asian summer monsoons: Reinterpreting cave speleothemδ18O

5. Southern Hemisphere forcing of South Asian monsoon precipitation over the past ~1 million years

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