Reconciling past changes in Earth's rotation with 20th century global sea-level rise: Resolving Munk's enigman

被引:50
|
作者
Mitrovica, Jerry X. [1 ]
Hay, Carling C. [1 ,2 ,3 ]
Morrow, Eric [2 ,3 ]
Kopp, Robert E. [2 ,3 ,4 ]
Dumberry, Mathieu [5 ,6 ]
Stanley, Sabine [7 ]
机构
[1] Harvard Univ, Dept Earth & Planetary Sci, 20 Oxford St, Cambridge, MA 02138 USA
[2] Rutgers State Univ, Dept Earth & Planetary Sci, Piscataway, NJ 08854 USA
[3] Rutgers State Univ, Inst Earth Ocean & Atmospher Sci, Piscataway, NJ 08854 USA
[4] Rutgers State Univ, Rutgers Energy Inst, Piscataway, NJ 08854 USA
[5] Univ Alberta, Dept Phys, Edmonton, AB T6G 2E1, Canada
[6] Univ Grenoble Alpes, ISTerre, F-38041 Grenoble, France
[7] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada
来源
SCIENCE ADVANCES | 2015年 / 1卷 / 11期
基金
美国海洋和大气管理局; 美国国家科学基金会; 加拿大自然科学与工程研究理事会;
关键词
INVERSION; DEGLACIATION; PLEISTOCENE; REANALYSIS; MODEL; AXIS;
D O I
10.1126/sciadv.1500679
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
In 2002, Munk defined an important enigma of 20th century global mean sea-level (GMSL) rise that has yet to be resolved. First, he listed three canonical observations related to Earth's rotation [(i) the slowing of Earth's rotation rate over the last three millennia inferred from ancient eclipse observations, and changes in the (ii) amplitude and (iii) orientation of Earth's rotation vector over the last century estimated from geodetic and astronomic measurements] and argued that they could all be fit by a model of ongoing glacial isostatic adjustment (GIA) associated with the last ice age. Second, he demonstrated that prevailing estimates of the 20th century GMSL rise (similar to 1.5 to 2.0 mm/year), after correction for the maximum signal from ocean thermal expansion, implied mass flux from ice sheets and glaciers at a level that would grossly misfit the residual GIA-corrected observations of Earth's rotation. We demonstrate that the combination of lower estimates of the 20th century GMSL rise (up to 1990) improved modeling of the GIA process and that the correction of the eclipse record for a signal due to angular momentum exchange between the fluid outer core and the mantle reconciles all three Earth rotation observations. This resolution adds confidence to recent estimates of individual contributions to 20th century sea-level change and to projections of GMSL rise to the end of the 21st century based on them.
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页数:6
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