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Expert judgements on the response of the Atlantic meridional overturning circulation to climate change

机译:关于大西洋经络翻转环流对气候变化的响应的专家判断

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摘要

We present results from detailed interviews with 12 leading climate scientists about the possible effects of global climate change on the Atlantic Meridional Overturning Circulation (AMOC). The elicitation sought to examine the range of opinions within the climatic research community about the physical processes that determine the current strength of the AMOC, its future evolution in a changing climate and the consequences of potential AMOC changes. Experts assign different relative importance to physical processes which determine the present-day strength of the AMOC as well as to forcing factors which determine its future evolution under climate change. Many processes and factors deemed important are assessed as poorly known and insufficiently represented in state-of-the-art climate models. All experts anticipate a weakening of the AMOC under scenarios of increase of greenhouse gas concentrations. Two experts expect a permanent collapse of the AMOC as the most likely response under a 4×CO2 scenario. Assuming a global mean temperature increase in the year 2100 of 4 K, eight experts assess the probability of triggering an AMOC collapse as significantly different from zero, three of them as larger than 40%. Elicited consequences of AMOC reduction include strong changes in temperature, precipitation distribution and sea level in the North Atlantic area. It is expected that an appropriately designed research program, with emphasis on long-term observations and coupled climate modeling, would contribute to substantially reduce uncertainty about the future evolution of the AMOC.
机译:我们提供了对12位主要气候科学家进行的详细访谈的结果,这些访谈涉及全球气候变化对大西洋子午线翻转循环(AMOC)的可能影响。这项启发旨在研究气候研究界内部关于决定AMOC当前强度,其在气候变化中的未来演变以及潜在AMOC变化后果的物理过程的观点。专家将不同的相对重要性分配给决定AMOC当前强度的物理过程以及确定气候变化下其未来演变的强迫因素。在最先进的气候模型中,许多被认为重要的过程和因素被评估为鲜为人知且代表性不足。所有专家预计,在温室气体浓度增加的情况下,AMOC将会减弱。两位专家预计,在4×CO2 情景下,AMOC的永久崩溃是最可能的反应。假设2100年全球平均温度升高4 K,八位专家评估触发AMOC崩溃的可能性与零显着不同,其中三位大于40%。减少AMOC的自发后果包括北大西洋地区温度,降水分布和海平面的强烈变化。预计适当设计的研究计划(重点在于长期观测和耦合的气候模拟)将有助于大大减少AMOC未来发展的不确定性。

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  • 来源
    《Climatic Change》 |2007年第4期|235-265|共31页
  • 作者单位

    School of Earth and Ocean Sciences University of Victoria PO Box 3055 STN CSC Victoria BC V8W3P6 Canada;

    Potsdam Institute for Climate Impact Research Potsdam Germany;

    Department of Engineering and Public Policy Carnegie Mellon University Pittsburgh CA USA;

    Potsdam Institute for Climate Impact Research Potsdam Germany;

    Potsdam Institute for Climate Impact Research Potsdam Germany;

    Department of Chemical and Petroleum Engineering University of Calgary Calgary Canada;

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