Irreversible climate change due to carbon dioxide emissions

被引:1963
作者
Solomon, Susan [1 ]
Plattner, Gian-Kasper [2 ]
Knutti, Reto [3 ]
Friedlingstein, Pierre [4 ]
机构
[1] Natl Ocean & Atmospher Adm, Earth Syst Res Lab, Div Chem Sci, Boulder, CO 80305 USA
[2] ETH, Inst Biogeochem & Pollutant Dynam, CH-8092 Zurich, Switzerland
[3] ETH, Inst Atmospher & Climate Sci, CH-8092 Zurich, Switzerland
[4] Univ Versailles St Quentin, Commissariat Energie Atom Saclay, CNRS,Unite Mixte Rech 1572, Lab Sci Climat & Environm,Inst Pierre Simon Lapla, F-91191 Gif Sur Yvette, France
关键词
dangerous interference; precipitation; sea level rise; warming; ICE-SHEET; PROJECTIONS; INCREASE; MODEL; OCEAN; 21ST-CENTURY; INTERFERENCE; CONSTRAINTS; SENSITIVITY; ATMOSPHERE;
D O I
10.1073/pnas.0812721106
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
The severity of damaging human-induced climate change depends not only on the magnitude of the change but also on the potential for irreversibility. This paper shows that the climate change that takes place due to increases in carbon dioxide concentration is largely irreversible for 1,000 years after emissions stop. Following cessation of emissions, removal of atmospheric carbon dioxide decreases radiative forcing, but is largely compensated by slower loss of heat to the ocean, so that atmospheric temperatures do not drop significantly for at least 1,000 years. Among illustrative irreversible impacts that should be expected if atmospheric carbon dioxide concentrations increase from current levels near 385 parts per million by volume (ppmv) to a peak of 450-600 ppmv over the coming century are irreversible dry-season rainfall reductions in several regions comparable to those of the "dust bowl'' era and inexorable sea level rise. Thermal expansion of the warming ocean provides a conservative lower limit to irreversible global average sea level rise of at least 0.4-1.0 m if 21st century CO2 concentrations exceed 600 ppmv and 0.6-1.9 m for peak CO2 concentrations exceeding approximate to 1,000 ppmv. Additional contributions from glaciers and ice sheet contributions to future sea level rise are uncertain but may equal or exceed several meters over the next millennium or longer.
引用
收藏
页码:1704 / 1709
页数:6
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