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Titlebook: Sea-Level Rise and Coastal Subsidence: Causes, Consequences, and Strategies; John D. Milliman,Bilal U. Haq Book 1996 Springer Science+Busi

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书目名称Sea-Level Rise and Coastal Subsidence: Causes, Consequences, and Strategies
编辑John D. Milliman,Bilal U. Haq
视频video
丛书名称Coastal Systems and Continental Margins
图书封面Titlebook: Sea-Level Rise and Coastal Subsidence: Causes, Consequences, and Strategies;  John D. Milliman,Bilal U. Haq Book 1996 Springer Science+Busi
描述Greenhouse-induced climate warming increasingly appears to be areality, and the warming climate will be accompanied by an acceleratedsea level rise - as much as 60-100 cm over the nextcentury. What is commonly absent in the discussion of rising sealevel, however, is the role played by the subsidence of low-lyingcoastal areas, which can have a far greater local effect than theeustatic rise of the sea. The combined sea-level rise and landsubsidence will almost certainly make the greatest impact on coastalsocieties in the densely populated regions of southern Asia, but itseffects will be felt globally. .This volume explores the concepts of sea-level rise and coastalsubsidence, both natural and anthropogenically accelerated, in theform of a series of case studies in such diverse locations as Bangkok,Bangladesh, Venice, and the Niger and Mississippi deltas, as well as adiscussion of the economic, engineering and policy responses that mustbe considered if the effects of local sea-level rise are to bemitigated.
出版日期Book 1996
关键词Delta; Sediment; Sedimentation; climate; erosion; climate change; ecotoxicology; hydrogeology
版次1
doihttps://doi.org/10.1007/978-94-015-8719-8
isbn_softcover978-90-481-4672-7
isbn_ebook978-94-015-8719-8Series ISSN 1384-6434
issn_series 1384-6434
copyrightSpringer Science+Business Media B.V. 1996
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978-90-481-4672-7Springer Science+Business Media B.V. 1996
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Sea-Level Rise and Coastal Subsidence: Causes, Consequences, and Strategies978-94-015-8719-8Series ISSN 1384-6434
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Land Subsidence in Coastal LowlandsCauses and ranges of coastal lowland subsidence are varied, but in general natural subsidence amounts to centimeters to a few meters per century, while human-induced subsidence can amount to meters in a few decades. As a result, coastal subsidence must be taken into account when predicting relative sea-level rise over the next century.
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Sea-Level Rise and the Stability of Barrier Islands, with special reference to the Wadden SeaChains of sand barrier islands are common morphologic features along many shores, occupying about 8% of the world’s coastlines. The Wadden Sea, which stretches along the eastern side of the North Sea, has one of the best studied barrier island systems in the world (Fig. 1).
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