全球变暖
海平面上升
气候学
环境科学
气候变化
气候突变
温室气体
大气(单位)
铅(地质)
大气科学
全球温度
全球变暖对海洋的影响
海平面
全球变暖的影响
海洋学
气象学
地理
地质学
地貌学
作者
Gerald A. Meehl,Warren M. Washington,William D. Collins,Julie M. Arblaster,Aixue Hu,Lawrence Buja,Gary Strand,Haiyan Teng
出处
期刊:Science
[American Association for the Advancement of Science (AAAS)]
日期:2005-03-18
卷期号:307 (5716): 1769-1772
被引量:679
标识
DOI:10.1126/science.1106663
摘要
Two global coupled climate models show that even if the concentrations of greenhouse gases in the atmosphere had been stabilized in the year 2000, we are already committed to further global warming of about another half degree and an additional 320% sea level rise caused by thermal expansion by the end of the 21st century. Projected weakening of the meridional overturning circulation in the North Atlantic Ocean does not lead to a net cooling in Europe. At any given point in time, even if concentrations are stabilized, there is a commitment to future climate changes that will be greater than those we have already observed.
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