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Coastal Erosion and Rising Sea-Level

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Sea-Level Rise and Coastal Subsidence

Part of the book series: Coastal Systems and Continental Margins ((CSCM,volume 2))

Abstract

Coastal erosion is facilitated by rising sea level, but it can also occur on coastlines where the sea level is stable or even falling. The modern prevalence of beach erosion on the world’s coastlines is not, therefore, an indication of global sea-level rise. However, if such a sea-level rise develops, perhaps as a consequence of the greenhouse effect, there will be an acceleration of existing beach erosion, and erosion will begin on many beaches that are now stable or growing. Accelerated erosion also will be seen on cliffs, deltas, coastal swamps, and developed coastlines. The changes predicted globally are already in evidence on sectors of the world’s coastline where land subsidence has produced a relative sea-level rise.

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Authors
  1. Eric C. F. Bird
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Editors and Affiliations

  1. School of Marine Science, College of William and Mary, 23062, Gloucester Point, Virginia, USA

    John D. Milliman

  2. 20816, Bethesda, Maryland, USA

    Bilal U. Haq

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© 1996 Springer Science+Business Media Dordrecht

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Bird, E.C.F. (1996). Coastal Erosion and Rising Sea-Level. In: Milliman, J.D., Haq, B.U. (eds) Sea-Level Rise and Coastal Subsidence. Coastal Systems and Continental Margins, vol 2. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8719-8_5

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  • DOI: https://doi.org/10.1007/978-94-015-8719-8_5

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-90-481-4672-7

  • Online ISBN: 978-94-015-8719-8

  • eBook Packages: Springer Book Archive

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