IOCAS-IR  > 海洋环流与波动重点实验室
Wind-driven sediment exchange between the Indian marginal seas over the last 18 000 years
Kang, Xiaoying1,5; Yu, Zhaojie1,2,3,4; Song, Lina1,3; Colin, Christophe6; Wilson, David J.7; Song, Zehua1; Su, Bai1; Tang, Xiaojie1,6; Chang, Fengming1; Bassinot, Franck8; Wan, Shiming1
2024-08-01
发表期刊ENVIRONMENTAL RESEARCH LETTERS
ISSN1748-9326
卷号19期号:8页码:11
通讯作者Yu, Zhaojie([email protected]) ; Song, Lina([email protected])
摘要The Indian Coastal Current is the only channel for material exchange between the two largest marginal seas in the northern Indian Ocean: the Bay of Bengal and the Arabian Sea. However, its past history is poorly known, limiting accurate predictions of its future changes. Here, we present a new clay mineral record from south of India supported by interpretations of model simulations to trace its variability over the last 18 000 years. Decreased smectite/(illite + chlorite) ratios during the cold intervals suggest that a stronger northeasterly wind led to a mean southward flow of the Indian Coastal Current in the Bay of Bengal. In contrast, increased smectite/(illite + chlorite) ratios during the warm intervals suggest the opposite scenario. Combining the proxy record with model simulations, we infer that atmospheric circulation changes were the main driver of the changes. Moreover, a possible link is observed between a positive Indian Ocean Dipole (IOD) and weakened southward flow of the Indian Coastal Current in the Bay of Bengal during the Holocene. These findings imply that future warming scenarios, if associated with more intense positive IOD events as proposed, may lead to a reduction in fresh water transport from the Bay of Bengal to the Arabian Sea.
关键词Northern Indian Ocean Indian Coastal Current clay minerals TraCE-21 model iTraCE model
DOI10.1088/1748-9326/ad5bf4
收录类别SCI
语种英语
资助项目National Natural Science Foundation of China[42376055]; National Natural Science Foundation of China[42176034]; National Natural Science Foundation of China[91958107]; Strategic Priority Research Program of Chinese Academy of Sciences[XDB42010402]; Natural Science Foundation of Shandong[ZR2022YQ33]; Youth Innovation Promotion Association, CAS[2020210]; National Key Research and Development Program of China[2022YFF0800503]; Natural Environment Research Council independent research fellowship[NE/T011440/1]; NCAR CISL
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
WOS类目Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS记录号WOS:001268027000001
出版者IOP Publishing Ltd
WOS关键词OCEAN DIPOLE EVENTS ; CLAY MINERAL DISTRIBUTION ; WESTERN BOUNDARY CURRENT ; COASTAL CURRENT ; ISOTOPIC COMPOSITIONS ; CONTINENTAL-MARGIN ; SURFACE SEDIMENTS ; LATE QUATERNARY ; RIVER SYSTEM ; ARABIAN SEA
引用统计
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/186315
专题海洋环流与波动重点实验室
通讯作者Yu, Zhaojie; Song, Lina
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Observat & Forecasting, Qingdao 266071, Peoples R China
2.Qingdao Marine Sci & Technol Ctr, Lab Marine Geol, Qingdao, Peoples R China
3.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China
4.Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao 266590, Peoples R China
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
6.Univ Paris Saclay, CNRS, GEOPS, F-91405 Orsay, France
7.Univ London, Univ Coll London & Birkbeck, Inst Earth & Planetary Sci, Gower St, London WC1 E6BT, England
8.Univ Paris Saclay, LSCE IPSL, CEA CNRS UVSQ, F-91191 Gif Sur Yvette, France
第一作者单位中国科学院海洋研究所
通讯作者单位中国科学院海洋研究所;  中国科学院海洋大科学研究中心
推荐引用方式
GB/T 7714
Kang, Xiaoying,Yu, Zhaojie,Song, Lina,et al. Wind-driven sediment exchange between the Indian marginal seas over the last 18 000 years[J]. ENVIRONMENTAL RESEARCH LETTERS,2024,19(8):11.
APA Kang, Xiaoying.,Yu, Zhaojie.,Song, Lina.,Colin, Christophe.,Wilson, David J..,...&Wan, Shiming.(2024).Wind-driven sediment exchange between the Indian marginal seas over the last 18 000 years.ENVIRONMENTAL RESEARCH LETTERS,19(8),11.
MLA Kang, Xiaoying,et al."Wind-driven sediment exchange between the Indian marginal seas over the last 18 000 years".ENVIRONMENTAL RESEARCH LETTERS 19.8(2024):11.
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