Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d
The Asian monsoon is an important component of the global climate system. Seasonal variations in wind, rainfall, and temperature associated with the Asian monsoon systems affect a vast expanse of tropical and subtropical Asia. Speleothem-derived summer monsoon variation ill East Asia was previously...
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ftchengkunguniv:oai:ir.lib.ncku.edu.tw:987654321/98122 2023-05-15T17:26:07+02:00 Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d Zhou, Houyun Zhao, Jianxin Zhang, Pingzhong Shen, Chuan-Chou Chi, Baoquan Feng, Yuexing Lin, Yin Guan, Huazheng You, Chen-Feng Earth Dynamic System Research Center 2008-09 https://doi.org/10.1016/j.yqres.2008.04.007 http://ir.lib.ncku.edu.tw/handle/987654321/98122 Eng en_US eng Elsevier Quaternary Research, Vol. 70, No. 2, pp. 315-321 Asian monsoon North Atlantic stalagmite paleoclimate millennial-scale event decoupling teleconnection marine oxygen isotope stage 5d 2008 ftchengkunguniv https://doi.org/10.1016/j.yqres.2008.04.007 2016-05-22T07:09:57Z The Asian monsoon is an important component of the global climate system. Seasonal variations in wind, rainfall, and temperature associated with the Asian monsoon systems affect a vast expanse of tropical and subtropical Asia. Speleothem-derived summer monsoon variation ill East Asia was previously found to be closely associated with millennial-scale change in temperature in the North Atlantic region between 75 and 10 ka. New evidence recovered from East Asia, however, suggests that the teleconnection between summer monsoon ill East Asia and temperature change in the North Atlantic region may have significantly reduced during 120 to - 110 ka, a period directly after the full last interglaciation and corresponding roughly to marine oxygen isotope stage 5d. This reduction may be due to the low ice volume in the North Hemisphere at that time, which makes the millennial-scale change in temperature in the North Atlantic region less effective in influencing the Asian Summer monsoon. This is important for investigating the mechanisms controlling the Asian Summer monsoon and the paleoclimatic teleconnection between East Asia and the North Atlantic region, and for predicting monsoon-associated precipitation in East Asia under a global-warming trend. (C) 2008 University of Washington. All rights reserved. Other/Unknown Material North Atlantic National Cheng Kung University: NCKU Institutional Repository Quaternary Research 70 2 315 321 |
institution |
Open Polar |
collection |
National Cheng Kung University: NCKU Institutional Repository |
op_collection_id |
ftchengkunguniv |
language |
English |
topic |
Asian monsoon North Atlantic stalagmite paleoclimate millennial-scale event decoupling teleconnection marine oxygen isotope stage 5d |
spellingShingle |
Asian monsoon North Atlantic stalagmite paleoclimate millennial-scale event decoupling teleconnection marine oxygen isotope stage 5d Zhou, Houyun Zhao, Jianxin Zhang, Pingzhong Shen, Chuan-Chou Chi, Baoquan Feng, Yuexing Lin, Yin Guan, Huazheng You, Chen-Feng Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d |
topic_facet |
Asian monsoon North Atlantic stalagmite paleoclimate millennial-scale event decoupling teleconnection marine oxygen isotope stage 5d |
description |
The Asian monsoon is an important component of the global climate system. Seasonal variations in wind, rainfall, and temperature associated with the Asian monsoon systems affect a vast expanse of tropical and subtropical Asia. Speleothem-derived summer monsoon variation ill East Asia was previously found to be closely associated with millennial-scale change in temperature in the North Atlantic region between 75 and 10 ka. New evidence recovered from East Asia, however, suggests that the teleconnection between summer monsoon ill East Asia and temperature change in the North Atlantic region may have significantly reduced during 120 to - 110 ka, a period directly after the full last interglaciation and corresponding roughly to marine oxygen isotope stage 5d. This reduction may be due to the low ice volume in the North Hemisphere at that time, which makes the millennial-scale change in temperature in the North Atlantic region less effective in influencing the Asian Summer monsoon. This is important for investigating the mechanisms controlling the Asian Summer monsoon and the paleoclimatic teleconnection between East Asia and the North Atlantic region, and for predicting monsoon-associated precipitation in East Asia under a global-warming trend. (C) 2008 University of Washington. All rights reserved. |
author2 |
Earth Dynamic System Research Center |
author |
Zhou, Houyun Zhao, Jianxin Zhang, Pingzhong Shen, Chuan-Chou Chi, Baoquan Feng, Yuexing Lin, Yin Guan, Huazheng You, Chen-Feng |
author_facet |
Zhou, Houyun Zhao, Jianxin Zhang, Pingzhong Shen, Chuan-Chou Chi, Baoquan Feng, Yuexing Lin, Yin Guan, Huazheng You, Chen-Feng |
author_sort |
Zhou, Houyun |
title |
Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d |
title_short |
Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d |
title_full |
Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d |
title_fullStr |
Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d |
title_full_unstemmed |
Decoupling of stalagmite-derived Asian summer monsoon records from North Atlantic temperature change during marine oxygen isotope stage 5d |
title_sort |
decoupling of stalagmite-derived asian summer monsoon records from north atlantic temperature change during marine oxygen isotope stage 5d |
publisher |
Elsevier |
publishDate |
2008 |
url |
https://doi.org/10.1016/j.yqres.2008.04.007 http://ir.lib.ncku.edu.tw/handle/987654321/98122 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Quaternary Research, Vol. 70, No. 2, pp. 315-321 |
op_doi |
https://doi.org/10.1016/j.yqres.2008.04.007 |
container_title |
Quaternary Research |
container_volume |
70 |
container_issue |
2 |
container_start_page |
315 |
op_container_end_page |
321 |
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1766117682187337728 |