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Retreat from a Rising SeaHard Choices in an Age of Climate Change$
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Orrin H. Pilkey, Linda Pilkey-Jarvis, and Keith C. Pilkey

Print publication date: 2016

Print ISBN-13: 9780231168441

Published to Columbia Scholarship Online: January 2017

DOI: 10.7312/columbia/9780231168441.001.0001

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PRINTED FROM COLUMBIA SCHOLARSHIP ONLINE (www.columbia.universitypressscholarship.com). (c) Copyright University of Minnesota Press, 2022. All Rights Reserved. An individual user may print out a PDF of a single chapter of a monograph in CUPSO for personal use.date: 17 May 2022

The Overflowing Ocean

The Overflowing Ocean

Chapter:
(p.11) 2 The Overflowing Ocean
Source:
Retreat from a Rising Sea
Author(s):

Orrin H. Pilkey

Linda Pilkey-Jarvis

Keith C. Pilkey

Publisher:
Columbia University Press
DOI:10.7312/columbia/9780231168441.003.0002

Summarizes the causes of sea-level rise; primarily these are warming and expansion in the upper 2,000 meters of the ocean, and melting of the ice sheets. The ice sheets are the most difficult aspect of sea-level rise to predict. There is a possibility of a catastrophic loss of ice from West Antarctica, leading to a sea-level rise of 10 feet by the end of the century. Although possible, this is highly unlikely. There is a strong tendency for communities to protect properties as the sea level rises. After each storm, cries arise for seawalls or beach replenishment. In the long term, seawalls destroy beaches and replenishment will become increasingly expensive with sea-level rise.

Keywords:   West Antarctic ice sheet, warming ocean, ice shelves, shoreline erosion, sea-level rise, beach replenishment, seawalls

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