Geographic Variability of Sea-Level Change

被引:86
作者
Kopp, Robert E. [1 ,2 ,3 ]
Hay, Carling C. [1 ,3 ,4 ]
Little, Christopher M. [5 ]
Mitrovica, Jerry X. [4 ]
机构
[1] Rutgers State Univ, Dept Earth & Planetary Sci, 610 Thylor Rd, Piscataway, NJ 08854 USA
[2] Rutgers State Univ, Rutgers Energy Inst, Brunswick, NJ 08901 USA
[3] Rutgers State Univ, Inst Earth Ocean & Atmospher Sci, New Brunswick, NJ 08901 USA
[4] Harvard Univ, Dept Earth & Planetary Sci, Cambridge, MA 02138 USA
[5] Atmospher & Environm Res Inc, Lexington, MA 02421 USA
基金
美国国家科学基金会;
关键词
Sea level; Ocean modeling; Glacial-isostatic adjustment; Sea-level fingerprints; Tide gauges; Satellite altimetry;
D O I
10.1007/s40641-015-0015-5
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Local sea-level changes differ significantly from global-mean sea-level change as a result of (1) non-climatic, geological background processes; (2) atmosphere/ocean dynamics; and (3) the gravitational, elastic, and rotational "fingerprint" effects of ice and ocean mass redistribution. Though the research communities working on these different effects each have a long history, the integration of all these different processes into interpretations of past changes and projections of future change is an active area of research. Fully characterizing the past contributions of these processes requires information from sources covering a range of timescales, including geological proxies, tide-gauge observations from the last similar to 3 centuries, and satellite-altimetry data from the last similar to 2 decades. Local sea-level rise projections must account for the different spatial patterns of different processes, as well as potential correlations between different drivers.
引用
收藏
页码:192 / 204
页数:13
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