Revisiting the Earth's sea-level and energy budgets from 1961 to 2008

被引:325
作者
Church, John A. [1 ]
White, Neil J. [1 ]
Konikow, Leonard F. [2 ]
Domingues, Catia M. [3 ]
Cogley, J. Graham [4 ]
Rignot, Eric [5 ,6 ]
Gregory, Jonathan M. [7 ,8 ]
van den Broeke, Michiel R. [9 ]
Monaghan, Andrew J. [10 ]
Velicogna, Isabella [5 ,6 ]
机构
[1] CSIRO Marine & Atmospher Res, Ctr Australian Weather & Climate Res & Wealth Oce, Hobart, Tas 7001, Australia
[2] US Geol Survey, Natl Ctr 431, Reston, VA 20192 USA
[3] CSIRO Marine & Atmospher Res, Antarctic Climate & Ecosyst Cooperat Res Ctr, Aspendale, Vic 3195, Australia
[4] Trent Univ, Dept Geog, Peterborough, ON K9J 7B8, Canada
[5] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA 92697 USA
[6] CALTECH, Jet Prop Lab, Pasadena, CA USA
[7] Univ Reading, Dept Meteorol, NCAS Climate, Reading RG6 6BB, Berks, England
[8] Hadley Ctr, Met Off, Exeter, Devon, England
[9] Univ Utrecht, Inst Marine & Atmospher Res, NL-3508 TA Utrecht, Netherlands
[10] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
关键词
CLIMATE-CHANGE; MASS-BALANCE; LAND WATER; OCEAN; HEAT; TRENDS; TEMPERATURE; IMPACT;
D O I
10.1029/2011GL048794
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We review the sea-level and energy budgets together from 1961, using recent and updated estimates of all terms. From 1972 to 2008, the observed sea-level rise (1.8 +/- 0.2 mm yr(-1) from tide gauges alone and 2.1 +/- 0.2 mm yr(-1) from a combination of tide gauges and altimeter observations) agrees well with the sum of contributions (1.8 +/- 0.4 mm yr(-1)) in magnitude and with both having similar increases in the rate of rise during the period. The largest contributions come from ocean thermal expansion (0.8 mm yr(-1)) and the melting of glaciers and ice caps (0.7 mm yr(-1)), with Greenland and Antarctica contributing about 0.4 mm yr(-1). The cryospheric contributions increase through the period (particularly in the 1990s) but the thermosteric contribution increases less rapidly. We include an improved estimate of aquifer depletion (0.3 mm yr(-1)), partially offsetting the retention of water in dams and giving a total terrestrial storage contribution of -0.1 mm yr(-1). Ocean warming (90% of the total of the Earth's energy increase) continues through to the end of the record, in agreement with continued greenhouse gas forcing. The aerosol forcing, inferred as a residual in the atmospheric energy balance, is estimated as -0.8 +/- 0.4 W m(-2) for the 1980s and early 1990s. It increases in the late 1990s, as is required for consistency with little surface warming over the last decade. This increase is likely at least partially related to substantial increases in aerosol emissions from developing nations and moderate volcanic activity. Citation: Church, J. A., N. J. White, L. F. Konikow, C. M. Domingues, J. G. Cogley, E. Rignot, J. M. Gregory, M. R. van den Broeke, A. J. Monaghan, and I. Velicogna (2011), Revisiting the Earth's sea-level and energy budgets from 1961 to 2008, Geophys. Res. Lett., 38, L18601, doi:10.1029/2011GL048794.
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页数:8
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