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dc.contributor.authorFitzGerald, Duncan M.  Concept link
dc.contributor.authorFenster, Michael S.  Concept link
dc.contributor.authorArgow, Britt A.  Concept link
dc.contributor.authorBuynevich, Ilya V.  Concept link
dc.date.accessioned2008-07-03T13:03:28Z
dc.date.available2008-07-03T13:03:28Z
dc.date.issued2007-06-28
dc.identifier.urihttps://hdl.handle.net/1912/2273
dc.descriptionAuthor Posting. © Annual Reviews, 2007. This is the author's version of the work. It is posted here by permission of Annual Reviews for personal use, not for redistribution. The definitive version was published in Annual Review of Earth and Planetary Sciences 36 (2008): 601-647, doi:10.1146/annurev.earth.35.031306.140139.en
dc.description.abstractRecent estimates by Intergovermental Panel on Climate Change (2007) are 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 it 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 on tidal deltas and erosion of adjacent barrier shorelines.en
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen
dc.relation.urihttps://doi.org/10.1146/annurev.earth.35.031306.140139
dc.subjectBarrier islandsen
dc.subjectTidal inletsen
dc.subjectSalt marshen
dc.subjectWetlandsen
dc.subjectInundationen
dc.subjectEstuariesen
dc.subjectEquilibrium slopeen
dc.titleCoastal impacts due to sea-level riseen
dc.typePreprinten


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