Modelling future sea-level change under greenhouse warming scenarios with an Earth system model of intermediate complexity

被引:0
作者
Makarynskyy, O [1 ]
Kuhn, M [1 ]
Featherstone, WE [1 ]
机构
[1] Curtin Univ Technol, Western Australian Ctr Geodesy, Perth, WA 6845, Australia
来源
GRAVITY, GEOID AND SPACE MISSIONS | 2005年 / 129卷
关键词
Earth system model; greenhouse gas scenario; global warming; sea-level change;
D O I
暂无
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Recently, a lot of effort has been put into estimating possible near-future changes (say, 10100 years) in the Earth's abiotic system, especially changes induced by human activities. One of the most studied issues is the effect of greenhouse gases on global warming and the corresponding change in sea-level around the world due to the associated deglaciation. This study focuses at projections of global sea-level changes on geological time scales. The University of Victoria's (Canada) coupled Earth System Climate Model of intermediate complexity was implemented. Two different greenhouse-warming scenarios were studied on timescales from hundreds to thousands years. The model was used to predict sea level variations under the combined influence of changes in sea ice coverage, global precipitation and evaporation, seawater salinity and temperature. Long-term projections show unequal water mass distribution over the globe: a sea-level rise of order of decimetres in equatorial and mid-latitude regions and a sea-level fall of up to 2 metres in polar regions, mostly around Antarctica.
引用
收藏
页码:260 / 265
页数:6
相关论文
共 29 条
  • [1] Simulating the ice-thickness distribution in a coupled climate model
    Bitz, CM
    Holland, MM
    Weaver, AJ
    Eby, M
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2001, 106 (C2) : 2441 - 2463
  • [2] A continuous climate-vegetation classification for use in climate-biosphere studies
    Brovkin, V
    Ganopolski, A
    Svirezhev, Y
    [J]. ECOLOGICAL MODELLING, 1997, 101 (2-3) : 251 - 261
  • [4] Earth system models of intermediate complexity: closing the gap in the spectrum of climate system models
    Claussen, M
    Mysak, LA
    Weaver, AJ
    Crucifix, M
    Fichefet, T
    Loutre, MF
    Weber, SL
    Alcamo, J
    Alexeev, VA
    Berger, A
    Calov, R
    Ganopolski, A
    Goosse, H
    Lohmann, G
    Lunkeit, F
    Mokhov, II
    Petoukhov, V
    Stone, P
    Wang, Z
    [J]. CLIMATE DYNAMICS, 2002, 18 (07) : 579 - 586
  • [5] DONATO GD, 2000, TECTONOPHYSICS, V320, P409
  • [6] Postglacial sea level: energy method
    Fang, M
    Hager, BH
    [J]. GLOBAL AND PLANETARY CHANGE, 1999, 20 (2-3) : 125 - 156
  • [7] An atmospheric energy-moisture balance model: Climatology, interpentadal climate change, and coupling to an ocean general circulation model
    Fanning, AF
    Weaver, AJ
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D10) : 15111 - 15128
  • [8] POSTGLACIAL SEA-LEVEL
    FARRELL, WE
    CLARK, JA
    [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1976, 46 (03): : 647 - 667
  • [9] SIMULATION OF THE LAST GLACIAL CYCLE BY A COUPLED, SECTORIALLY AVERAGED CLIMATE-ICE SHEET MODEL .2. RESPONSE TO INSOLATION AND CO2 VARIATIONS
    GALLEE, H
    VANYPERSELE, JP
    FICHEFET, T
    MARSIAT, I
    TRICOT, C
    BERGER, A
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1992, 97 (D14) : 15713 - 15740
  • [10] EXCITATION OF THE EARTHS ROTATIONAL AXIS BY RECENT GLACIAL DISCHARGES
    GASPERINI, P
    SABADINI, R
    YUEN, DA
    [J]. GEOPHYSICAL RESEARCH LETTERS, 1986, 13 (06) : 533 - 536