Mapping the return periods of extreme sea levels: Allowing for short sea level records, seasonality, and climate change

被引:27
|
作者
Bernier, N. B. [1 ]
Thompson, K. R.
Ou, J.
Ritchie, H.
机构
[1] Dalhousie Univ, Dept Oceanog, Halifax, NS B3H 4J1, Canada
[2] Meteorol Serv Canada, Dartmouth, NS B2Y 2N6, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
sea level; extremal analysis; storm surges; spatial mapping of coastal flooding; Digital Elevation Model; climate change;
D O I
10.1016/j.gloplacha.2006.11.027
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
This study of extreme sea levels is motivated by concern over increased coastal erosion and flooding under plausible climate change scenarios. Extremal analyses are performed on the annual and seasonal maxima from 24 tide gauge stations in the Northwest Atlantic. At data poor locations, a 40 yr surge hindcast and information from short observation records are used to reconstruct sea level records prior to the annual and seasonal analysis of extremes. A Digital Elevation Model is used to generate spatial maps of the return period of extreme sea levels associated with specified flooding probabilities under current conditions and under projected global sea level rise scenarios for the next century. It is the first time such maps have been produced. Their primary advantage is that extreme sea levels are expressed in terns of inundated areas as opposed to a critical flood value about an arbitrary datum. Another novel aspect of this study is that the extremal analyses are carried out for specific seasons. (c) 2006 Elsevier B.V All rights reserved.
引用
收藏
页码:139 / 150
页数:12
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