Impact of Sea Level Rise on Storm Surges around the Changjiang Estuary
The potential impacts of sea level rise (SLR) on storm surge around the Changjiang Estuary and the Hangzhou Bay are investigated using a shallow-water circulation model ADCIRC coupled with a spectral wave model SWAN. The validated model is applied to two typical typhoons under three scenarios: 1.0 m...
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| Veröffentlicht in: | Journal of coastal research 2014-10, Vol.SI (68), p.27-27 |
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| creator | Zhao, Changjin Ge, Jianzhong Ding, Pingxing |
| description | The potential impacts of sea level rise (SLR) on storm surge around the Changjiang Estuary and the Hangzhou Bay are investigated using a shallow-water circulation model ADCIRC coupled with a spectral wave model SWAN. The validated model is applied to two typical typhoons under three scenarios: 1.0 m SLR, 0.483 m SLR and present sea-level condition. In consideration of interactions of tide, waves and surge, the impact exerted by SLR on tide and waves are also discussed. The migration of the amphidromes generated by SLR causes the cophase lines to defect relatively counterclockwise near the Changjiang Estuary. Comparing the maximum wave height between each scenario, the wave height increase is found to be significant in shallow areas due to the increase in water depth. The breaking locations of the wave shift shoreward. The general patterns in wave height change are approximately determined by the typhoon path and topography. Taking the value of SLR into account, the peak of elevation near shore could experience a significant increase in the future. |
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The validated model is applied to two typical typhoons under three scenarios: 1.0 m SLR, 0.483 m SLR and present sea-level condition. In consideration of interactions of tide, waves and surge, the impact exerted by SLR on tide and waves are also discussed. The migration of the amphidromes generated by SLR causes the cophase lines to defect relatively counterclockwise near the Changjiang Estuary. Comparing the maximum wave height between each scenario, the wave height increase is found to be significant in shallow areas due to the increase in water depth. The breaking locations of the wave shift shoreward. The general patterns in wave height change are approximately determined by the typhoon path and topography. Taking the value of SLR into account, the peak of elevation near shore could experience a significant increase in the future.</description><identifier>ISSN: 0749-0208</identifier><identifier>EISSN: 1551-5036</identifier><language>eng</language><publisher>Fort Lauderdale: Allen Press Inc</publisher><subject>Brackish ; Climate change ; Elevation ; Estuaries ; Floods ; Global warming ; Marine ; Migration ; Sea level ; Sea level rise ; Shallow water ; Spectra ; Storm surges ; Tidal waves ; Tides ; Topography ; Typhoons ; Water circulation ; Water depth ; Wave height</subject><ispartof>Journal of coastal research, 2014-10, Vol.SI (68), p.27-27</ispartof><rights>Copyright Allen Press Publishing Services Fall 2014</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784</link.rule.ids></links><search><creatorcontrib>Zhao, Changjin</creatorcontrib><creatorcontrib>Ge, Jianzhong</creatorcontrib><creatorcontrib>Ding, Pingxing</creatorcontrib><title>Impact of Sea Level Rise on Storm Surges around the Changjiang Estuary</title><title>Journal of coastal research</title><description>The potential impacts of sea level rise (SLR) on storm surge around the Changjiang Estuary and the Hangzhou Bay are investigated using a shallow-water circulation model ADCIRC coupled with a spectral wave model SWAN. 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The validated model is applied to two typical typhoons under three scenarios: 1.0 m SLR, 0.483 m SLR and present sea-level condition. In consideration of interactions of tide, waves and surge, the impact exerted by SLR on tide and waves are also discussed. The migration of the amphidromes generated by SLR causes the cophase lines to defect relatively counterclockwise near the Changjiang Estuary. Comparing the maximum wave height between each scenario, the wave height increase is found to be significant in shallow areas due to the increase in water depth. The breaking locations of the wave shift shoreward. The general patterns in wave height change are approximately determined by the typhoon path and topography. Taking the value of SLR into account, the peak of elevation near shore could experience a significant increase in the future.</abstract><cop>Fort Lauderdale</cop><pub>Allen Press Inc</pub><tpages>1</tpages></addata></record> |
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| subjects | Brackish Climate change Elevation Estuaries Floods Global warming Marine Migration Sea level Sea level rise Shallow water Spectra Storm surges Tidal waves Tides Topography Typhoons Water circulation Water depth Wave height |
| title | Impact of Sea Level Rise on Storm Surges around the Changjiang Estuary |
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