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Coastal Impacts Due to Sea-Level Rise

The Intergovernmental Panel on Climate Change (2007) recently estimated that global sea level will rise from 0.18 to 0.59 m by the end of this century. Rising sea level not only inundates low-lying coastal regions but also contributes to the redistribution of sediment along sandy coasts. Over the lo...

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Bibliographic Details
Published in:Annual review of earth and planetary sciences 2008-01, Vol.36 (1), p.601-647
Main Authors: FitzGerald, Duncan M, Fenster, Michael S, Argow, Britt A, Buynevich, Ilya V
Format: Article
Language:English
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Summary:The Intergovernmental Panel on Climate Change (2007) recently estimated that global sea level will rise from 0.18 to 0.59 m by the end of this century. Rising sea level not only inundates low-lying coastal regions but also contributes to the redistribution of sediment along sandy coasts. Over the long term, sea-level rise (SLR) causes barrier islands to migrate landward while conserving mass through offshore and onshore sediment transport. Under these conditions, coastal systems adjust to SLR dynamically while maintaining a characteristic geometry that is unique to a particular coast. Coastal marshes are susceptible to accelerated SLR because their vertical accretion rates are limited and they may drown. As marshes convert to open water, tidal exchange through inlets increases, which leads to sand sequestration in tidal deltas and erosion of adjacent barrier shorelines.
ISSN:0084-6597
1545-4495
DOI:10.1146/annurev.earth.35.031306.140139