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21st century changes in the European climate: uncertainties derived from an ensemble of regional climate model simulations

机译:21世纪欧洲气候的变化:来自区域气候模型模拟整体的不确定性

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摘要

Seasonal mean temperature, precipitation and wind speed over Europe are analysed in an ensemble of 16 regional climate model (RCM) simulations for 1961-2100. The RCM takes boundary conditions from seven global climate models (GCMs) under four emission scenarios. One GCM was run three times under one emission scenario differing only in initial conditions. The ensemble is used to; (ⅰ) evaluate the simulated climate for 1961-1990, (ⅱ) assess future climate change and (ⅲ) illustrate uncertainties in future climate change related to natural variability, boundary conditions and emissions. Biases in the 1961-1990 period are strongly related to errors in the large-scale circulation in the GCMs. Significant temperature increases are seen for all of Europe already in the next decades. Precipitation increases in northern and decreases in southern Europe with a zone in between where the sign of change is uncertain. Wind speed decreases in many areas with exceptions in the northern seas and in parts of the Mediterranean in summer. Uncertainty largely depends on choice of GCM and their representation of changes in the large-scale circulation. The uncertainty related to forcing is most important by the end of the century while natural variability sometimes dominates the uncertainty in the nearest few decades.
机译:在1961-2100年的16个区域气候模型(RCM)模拟合集中分析了欧洲的季节性平均温度,降水和风速。 RCM从四种排放情景下的七个全球气候模型(GCM)中获取边界条件。一个GCM在一种排放情景下运行了三次,仅在初始条件下有所不同。合奏习惯于: (ⅰ)评估1961-1990年的模拟气候,(ⅱ)评估未来的气候变化,(ⅲ)说明与自然变异性,边界条件和排放有关的未来气候变化的不确定性。 1961-1990年期间的偏差与GCM大规模循环中的误差密切相关。在接下来的几十年中,整个欧洲的气温都将出现明显上升。北部的降水增加,而南部的降水减少,其间有一个变化迹象不确定的区域。除北部海域和夏季地中海部分地区外,许多地区的风速均下降。不确定性在很大程度上取决于GCM的选择及其在大规模流通中变化的表示形式。与强迫有关的不确定性在本世纪末最为重要,而自然可变性有时在最近的几十年中占主导地位。

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  • 来源
    《Tellus》 |2011年第1期|p.24-40|共17页
  • 作者单位

    Rossby Centre, Swedish Meteorological and Hydrological Institute, SE 601 96 Norrkoeping, Sweden;

    rnRossby Centre, Swedish Meteorological and Hydrological Institute, SE 601 96 Norrkoeping, Sweden;

    rnRossby Centre, Swedish Meteorological and Hydrological Institute, SE 601 96 Norrkoeping, Sweden;

    rnRossby Centre, Swedish Meteorological and Hydrological Institute, SE 601 96 Norrkoeping, Sweden;

    rnRossby Centre, Swedish Meteorological and Hydrological Institute, SE 601 96 Norrkoeping, Sweden;

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