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Modelling the increased frequency of extreme sea levels in the Ganges–Brahmaputra–Meghna delta due to sea level rise and other effects of climate change

Modelling the increased frequency of extreme sea levels in the Ganges–Brahmaputra–Meghna delta due to sea level rise and other effects of climate change
Modelling the increased frequency of extreme sea levels in the Ganges–Brahmaputra–Meghna delta due to sea level rise and other effects of climate change
Coastal flooding due to storm surge and high tides is a serious risk for inhabitants of the Ganges–Brahmaputra–Meghna (GBM) delta, as much of the land is close to sea level. Climate change could lead to large areas of land being subject to increased flooding, salinization and ultimate abandonment in West Bengal, India, and Bangladesh. IPCC 5th assessment modelling of sea level rise and estimates of subsidence rates from the EU IMPACT2C project suggest that sea level in the GBM delta region may rise by 0.63 to 0.88 m by 2090, with some studies suggesting this could be up to 0.5 m higher if potential substantial melting of the West Antarctic ice sheet is included. These sea level rise scenarios lead to increased frequency of high water coastal events. Any effect of climate change on the frequency and severity of storms can also have an effect on extreme sea levels. A shelf-sea model of the Bay of Bengal has been used to investigate how the combined effect of sea level rise and changes in other environmental conditions under climate change may alter the frequency of extreme sea level events for the period 1971 to 2099. The model was forced using atmospheric and oceanic boundary conditions derived from climate model projections and the future scenario increase in sea level was applied at its ocean boundary. The model results show an increased likelihood of extreme sea level events through the 21st century, with the frequency of events increasing greatly in the second half of the century: water levels that occurred at decadal time intervals under present-day model conditions occurred in most years by the middle of the 21st century and 3–15 times per year by 2100. The heights of the most extreme events tend to increase more in the first half of the century than the second. The modelled scenarios provide a case study of how sea level rise and other effects of climate change may combine to produce a greatly increased threat to life and property in the GBM delta by the end of this century.
2050-7887
1311-1322
Kay, S.
48a2ee19-d372-4a6b-9e0f-3be837de26cf
Caesar, J.
385614c7-1523-410a-9a04-61217ae10d10
Wolf, J.
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Bricheno, L.
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Nicholls, R.J.
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Saiful Islam, A.K.M.
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Haque, A.
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Pardeans, A.
73895aff-8a19-465b-a027-e0ae6584ef2c
Lowe, J.
6f434b48-eb86-42cd-9173-eeb081a41a25
Kay, S.
48a2ee19-d372-4a6b-9e0f-3be837de26cf
Caesar, J.
385614c7-1523-410a-9a04-61217ae10d10
Wolf, J.
13cf5067-f460-4851-9a09-d6bf7efe575b
Bricheno, L.
3a658e49-8b37-4ade-b743-78b42d636def
Nicholls, R.J.
4ce1e355-cc5d-4702-8124-820932c57076
Saiful Islam, A.K.M.
9b63ca9e-7d6e-49ab-976e-6c3c417b2466
Haque, A.
84bb42e7-f5a1-4e85-8ece-add5dafbe927
Pardeans, A.
73895aff-8a19-465b-a027-e0ae6584ef2c
Lowe, J.
6f434b48-eb86-42cd-9173-eeb081a41a25

Kay, S., Caesar, J., Wolf, J., Bricheno, L., Nicholls, R.J., Saiful Islam, A.K.M., Haque, A., Pardeans, A. and Lowe, J. (2015) Modelling the increased frequency of extreme sea levels in the Ganges–Brahmaputra–Meghna delta due to sea level rise and other effects of climate change. Environmental Science: Processes & Impacts, 17 (7), 1311-1322. (doi:10.1039/c4em00683f).

Record type: Article

Abstract

Coastal flooding due to storm surge and high tides is a serious risk for inhabitants of the Ganges–Brahmaputra–Meghna (GBM) delta, as much of the land is close to sea level. Climate change could lead to large areas of land being subject to increased flooding, salinization and ultimate abandonment in West Bengal, India, and Bangladesh. IPCC 5th assessment modelling of sea level rise and estimates of subsidence rates from the EU IMPACT2C project suggest that sea level in the GBM delta region may rise by 0.63 to 0.88 m by 2090, with some studies suggesting this could be up to 0.5 m higher if potential substantial melting of the West Antarctic ice sheet is included. These sea level rise scenarios lead to increased frequency of high water coastal events. Any effect of climate change on the frequency and severity of storms can also have an effect on extreme sea levels. A shelf-sea model of the Bay of Bengal has been used to investigate how the combined effect of sea level rise and changes in other environmental conditions under climate change may alter the frequency of extreme sea level events for the period 1971 to 2099. The model was forced using atmospheric and oceanic boundary conditions derived from climate model projections and the future scenario increase in sea level was applied at its ocean boundary. The model results show an increased likelihood of extreme sea level events through the 21st century, with the frequency of events increasing greatly in the second half of the century: water levels that occurred at decadal time intervals under present-day model conditions occurred in most years by the middle of the 21st century and 3–15 times per year by 2100. The heights of the most extreme events tend to increase more in the first half of the century than the second. The modelled scenarios provide a case study of how sea level rise and other effects of climate change may combine to produce a greatly increased threat to life and property in the GBM delta by the end of this century.

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Kay_et_al_SeaLevelRise_GBM_delta_ESPI_accepted.pdf - Accepted Manuscript
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Accepted/In Press date: 5 June 2015
e-pub ahead of print date: 5 June 2015
Published date: 1 July 2015
Organisations: Marine Systems Modelling, Energy & Climate Change Group

Identifiers

Local EPrints ID: 378733
URI: http://eprints.soton.ac.uk/id/eprint/378733
ISSN: 2050-7887
PURE UUID: f2455ee4-8471-48f4-bf5d-c0d80128f694
ORCID for R.J. Nicholls: ORCID iD orcid.org/0000-0002-9715-1109

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Date deposited: 20 Jul 2015 10:06
Last modified: 15 Mar 2024 03:18

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Contributors

Author: S. Kay
Author: J. Caesar
Author: J. Wolf
Author: L. Bricheno
Author: R.J. Nicholls ORCID iD
Author: A.K.M. Saiful Islam
Author: A. Haque
Author: A. Pardeans
Author: J. Lowe

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