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GLOBAL CHANGES IN THE SEA ICE COVER AND ASSOCIATED SURFACE TEMPERATURE CHANGES

机译:海冰盖的全球变化和相关表面温度变化

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The trends in the sea ice cover in the two hemispheres have been observed to be asymmetric with the rate of change in the Arctic being negative at -3.8% per decade while that of the Antarctic is positive at 1.7% per decade. These observations are confirmed in this study through analyses of a more robust data set that has been enhanced for better consistency and updated for improved statistics. With reports of anthropogenic global warming such phenomenon appears physically counter intuitive but trend studies of surface temperature over the same time period show the occurrence of a similar asymmetry. Satellite surface temperature data show that while global warming is strong and dominant in the Arctic, it is relatively minor in the Antarctic with the trends in sea ice covered areas and surrounding ice free regions observed to be even negative. A strong correlation of ice extent with surface temperature is observed, especially during the growth season, and the observed trends in the sea ice cover are coherent with the trends in surface temperature. The trend of global averages of the ice cover is negative but modest and is consistent and compatible with the positive but modest trend in global surface temperature. A continuation of the trend would mean the disappearance of summer ice by the end of the century but modelling projections indicate that the summer ice could be salvaged if anthropogenic greenhouse gases in the atmosphere are kept constant at the current level.
机译:在两个半球的海冰覆盖的趋势已经观察到不对称的北极是负面变化的以每十年-3.8%的税率,而南极是在每十年1.7%的阳性。这些观察证实了这项研究,通过已增强了更好的一致性和更新改善的统计数据更强大的数据集的分析。随着人为的全球变暖这样的现象出现报告在同一时间段表面温度的物理直觉,但趋势的研究显示了类似的不对称性的发生。卫星表面温度的数据显示,尽管全球变暖是强大的,并在北极占主导地位,它是相对较小的南极与海冰覆盖的区域的趋势和周围结冰的区域观察到甚至是负的。冰程度与表面温度的强相关性,观察到,特别是在生长季节,并在海冰盖观察到的趋势与在表面温度趋势相干的。覆冰的世界平均水平的趋势是负的,但谦虚是一致的,并与全球表面温度积极的,但温和的趋势一致。该趋势继续下去,将意味着夏治冰的消失在本世纪结束,但模拟预测表明,如果大气中的人为温室气体在目前的水平保持不变的夏治冰可以挽救。

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