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Contributions of a Strengthened Early Holocene Monsoon and Sediment Loading to Present-Day Subsidence of the Ganges-Brahmaputra Delta

文献类型:期刊论文

作者Ballu, V.1; Krien, Y.1; Becker, M.1; Goodbred, S.2; Spada, G.3; Shum, C. K.5,6; Calmant, S.4; Khan, Z.7; Karpytchev, M.1
刊名GEOPHYSICAL RESEARCH LETTERS
出版日期2018-02-16
卷号45期号:3页码:1433-1442
ISSN号0094-8276
DOI10.1002/2017GL076388
英文摘要The contribution of subsidence to relative sea level rise in the Ganges-Brahmaputra delta (GBD) is largely unknown and may considerably enhance exposure of the Bengal Basin populations to sea level rise and storm surges. This paper focuses on estimating the present-day subsidence induced by Holocene sediment in the Bengal Basin and by oceanic loading due to eustatic sea level rise over the past 18 kyr. Using a viscoelastic Earth model and sediment deposition history based on in situ measurements, results suggest that massive sediment influx initiated in the early Holocene under a strengthened South Asian monsoon may have contributed significantly to the present-day subsidence of the GBD. We estimate that the Holocene loading generates up to 1.6 mm/yr of the present-day subsidence along the GBD coast, depending on the rheological model of the Earth. This rate is close to the twentieth century global mean sea level rise (1.1-1.7 mm/yr). Thus, past climate change, by way of enhanced sedimentation, is impacting vulnerability of the GBD populations. Plain Language Summary This paper estimates the land subsidence induced by sediments deposited in the Bengal Basin and by the sea level rise over the past 18,000 years. The results of numerical modeling demonstrate that the coast of the Ganges-Brahmaputra delta subsides at a rate of about 1-1.6 mm/yr depending on the lithospheric thickness and the Earth mantle viscosity. This is comparable to the rate of global mean sea level rise during the twentieth century. Thus, the intense sedimentation generated by climate changes in the past contributes significantly to the present-day subsidence of the Bengal coast.
资助项目Belmont Forum/IGFA G8 Coastal Vulnerability Program ; BanD-AID project via ANR in France ; NSF in the United States ; DFG in Germany ; CSIRO/ARC in Australia ; DisPeA research grant
WOS研究方向Geology
语种英语
WOS记录号WOS:000426161800029
出版者AMER GEOPHYSICAL UNION
源URL[http://202.127.146.157/handle/2RYDP1HH/4699]  
专题中国科学院武汉植物园
通讯作者Karpytchev, M.
作者单位1.Univ La Rochelle, CNRS, LIENSs, UMR 7266, La Rochelle, France
2.Vanderbilt Univ, Dept Earth & Environm Sci, 221 Kirkland Hall, Nashville, TN 37235 USA
3.Univ Urbino Carlo Bo, Dipartimento Sci Pure & Appl, Urbino, Italy
4.UPS, IRD, CNES, CNRS,LEGOS UMR5566, Toulouse, France
5.Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA
6.Chinese Acad Sci, Inst Geodesy & Geophys, Wuhan, Hubei, Peoples R China
7.Inst Water Modelling, Dhaka, Bangladesh
推荐引用方式
GB/T 7714
Ballu, V.,Krien, Y.,Becker, M.,et al. Contributions of a Strengthened Early Holocene Monsoon and Sediment Loading to Present-Day Subsidence of the Ganges-Brahmaputra Delta[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(3):1433-1442.
APA Ballu, V..,Krien, Y..,Becker, M..,Goodbred, S..,Spada, G..,...&Karpytchev, M..(2018).Contributions of a Strengthened Early Holocene Monsoon and Sediment Loading to Present-Day Subsidence of the Ganges-Brahmaputra Delta.GEOPHYSICAL RESEARCH LETTERS,45(3),1433-1442.
MLA Ballu, V.,et al."Contributions of a Strengthened Early Holocene Monsoon and Sediment Loading to Present-Day Subsidence of the Ganges-Brahmaputra Delta".GEOPHYSICAL RESEARCH LETTERS 45.3(2018):1433-1442.

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来源:武汉植物园

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