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Regional climate change experiments over southern South America. II: Climate change scenarios in the late twenty-first century

机译:南美南部地区气候变化实验。 II:二十一世纪末的气候变化情景

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摘要

We present an analysis of climate change over southern South America as simulated by a regional climate model. The regional model MM5 was nested within time-slice global atmospheric model experiments conducted by the HadAM3H model. The simulations cover a 10-year period representing present-day climate (1981-1990) and two future scenarios for the SRESA2 and B2 emission scenarios for the period 2081-2090. There are a few quantitative differences between the two regional scenarios. The simulated changes are larger for the A2 than the B2 scenario, although with few qualitative differences. For the two regional scenarios, the warming in southern Brazil, Paraguay, Bolivia and northeastern Argentina is particularly large in spring. Over the western coast of South America both scenarios project a general decrease in precipitation. Both the A2 and B2 simulations show a general increase in precipitation in northern and central Argentina especially in summer and fall and a general decrease in precipitation in winter and spring. In fall the simulations agree on a general decrease in precipitation in southern Brazil. This reflects changes in the atmospheric circulationrnduring winter and spring. Changes in mean sea level pressure show a cell of increasing pressure centered somewhere in the southern Atlantic Ocean and southern Pacific Ocean, mainly during summer and fall in the Atlantic and in spring in the Pacific. In relation to the pressure distribution in the control run, this indicates a southward extension of the summer mean Atlantic and Pacific subtropical highs.
机译:我们通过区域气候模型对南美南部的气候变化进行了分析。区域模型MM5嵌套在HadAM3H模型进行的时间切片全球大气模型实验中。模拟涵盖了代表当前气候(1981-1990年)的10年时间段以及2081-2090年期间SRESA2和B2排放情景的两个未来情景。两种区域情景之间在数量上存在一些差异。尽管几乎没有定性差异,但A2的模拟变化比B2情景大。对于这两个区域情景,春季巴西南部,巴拉圭,玻利维亚和阿根廷东北部的变暖特别大。在南美的西海岸,这两种情况都表明降水普遍减少。 A2和B2模拟均显示阿根廷北部和中部的降水普遍增加,尤其是在夏季和秋季,冬季和春季的降水普遍减少。在秋季,模拟结果表明巴西南部的降水普遍减少。这反映了冬季和春季的大气环流变化。平均海平面压力的变化表明,一个压力不断增加的单元集中在南部大西洋和南部太平洋的某个地方,主要发生在夏季和秋季的大西洋以及春季的太平洋。关于控制运行中的压力分布,这表明夏季平均大西洋和太平洋副热带高压向南延伸。

著录项

  • 来源
    《Climate dynamics》 |2009年第8期|1081-1095|共15页
  • 作者单位

    Centro de Investigaciones del Mar y la Atmosfera (CIMA-CONICET/UBA) DCAO (FCEyN-UBA), Ciudad Universitaria, Pabellon II, Piso 2, 1428 Buenos Aires, Argentina;

    Centro de Investigaciones del Mar y la Atmosfera (CIMA-CONICET/UBA) DCAO (FCEyN-UBA), Ciudad Universitaria, Pabellon II, Piso 2, 1428 Buenos Aires, Argentina;

    Centro de Investigaciones del Mar y la Atmosfera (CIMA-CONICET/UBA), Ciudad Universitaria, Pabellon II, Piso 2, 1428 Buenos Aires, Argentina;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    regional climate modeling; Southern South America; climate change scenarios;

    机译:区域气候模拟;南美南部;气候变化情景;

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