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首页> 外文期刊>Geophysical Research Letters >Climate change scenarios for seasonal precipitation in South America from IPCC-AR4 models
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Climate change scenarios for seasonal precipitation in South America from IPCC-AR4 models

机译:IPCC-AR4模型在南美季节性降水的气候变化情景中

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A subset of climate simulations of the 20th century from the IPCC-AR4 is analyzed to assess the ability of these models to reproduce the observed climatological seasonal precipitation in South America during the period 1970 1999. Changes of the model climatology in a climate change scenario (SRESA1b) for the period 2070 - 2099 are also discussed. Results show that models are able to reproduce the main features of the precipitation seasonal cycle over South America, although the precipitation in the SACZ region and the precipitation maximum over southeastern South America observed during the cold season are not well-represented. There is a general consensus among models that the precipitation changes projected are mainly: i) an increase of summer precipitation over southeastern subtropical South America; ii) a reduction of winter precipitation over most of the continent; and iii) reduction of precipitation in all seasons along the southern Andes.
机译:分析了来自IPCC-AR4的20世纪气候模拟的一个子集,以评估这些模型再现1970 1999年南美洲观测到的气候季节性降水的能力。气候变化情景中模型气候的变化(还讨论了2070年至2099年的SRESA1b)。结果表明,尽管在寒冷季节观测到的SACZ地区的降水和南美洲东南部的最大降水量没有得到很好的反映,但这些模型能够再现南美洲降水季节周期的主要特征。在模型之间普遍有一个共识,即预测的降水变化主要是:i)东南亚热带南美夏季降水的增加; ii)减少非洲大陆大部分地区的冬季降水; iii)减少安第斯山脉南部所有季节的降水。

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