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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Comparative analysis of the ability of a set of CMIP3 and CMIP5 global climate models to represent precipitation in South America
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Comparative analysis of the ability of a set of CMIP3 and CMIP5 global climate models to represent precipitation in South America

机译:一组CMIP3和CMIP5全球气候模型代表南美降水的能力的比较分析

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摘要

The purpose of this study is to evaluate the ability of two sets of global climate models (GCMs) derived from the Coupled Model Intercomparison Projects Phase 3 (CMIP3) and Phase 5 (CMIP5) to represent the summer, winter, and annual precipitation mean patterns in South America south of the equator and in three particular sub-regions, between years 1960 and 1999. Different metrics (relative bias, spatial correlation, RMSE, and relative errors) were calculated and compared between both projects to determine if there has been improvement from CMIP3 to CMIP5 models in the representation of regional rainfall. Results from this analysis indicate that for the analysed seasons, precipitation simulated by both CMIP3 and CMIP5 models' ensembles exhibited some differences. In DJF, the relative bias over Amazonia, central South America, eastern Argentina, and Uruguay is reduced in CMIP5 compared with CMIP3. In JJA, the same occurs in some areas of Amazonia. Annual precipitation is also better represented by the CMIP5 than CMIP3 GCMs as they underestimate precipitation to a lesser extent, although in NE Brazil the overestimation values are much larger in CMIP5 than in CMIP3 analysis. In line with previous studies, the multi-model ensembles show the best representation of the observed patterns in most seasons and regions. Only in some cases, single GCMs [MIROC3.2(hires)-CMIP3- and MIROC4h-CMIP5] presented better results than the ensemble. The high horizontal resolution of these models suggests that this could be a relevant issue for a more adequate estimation of rainfall at least in the analysed regions.
机译:这项研究的目的是评估从耦合模型比较项目第3阶段(CMIP3)和第5阶段(CMIP5)导出的两组全球气候模型(GCM)代表夏季,冬季和年降水均值模式的能力在1960年至1999年之间的南美赤道以南和三个特定子区域中。计算了不同的指标(相对偏差,空间相关性,RMSE和相对误差),并在两个项目之间进行了比较,以确定是否有所改善从CMIP3到CMIP5模型来表示区域降雨。该分析结果表明,在所分析的季节中,由CMIP3和CMIP5模型的集合模拟的降水表现出一些差异。在DJF中,与CMIP3相比,CMIP5在Amazonia,南美中部,阿根廷东部和乌拉圭的相对偏倚有所减少。在JJA中,在Amazonia的某些地区也是如此。 CMIP5比CMIP3 GCM更能代表年降水量,因为它们低估了降水的程度,尽管在巴西东北部,CMIP5的高估值比CMIP3分析的高得多。与以前的研究一致,多模型合奏在大多数季节和地区都可以很好地表示观测到的模式。仅在某些情况下,单个GCM [MIROC3.2(hires)-CMIP3-和MIROC4h-CMIP5]呈现出比集合更好的结果。这些模型的高水平分辨率表明,这可能是一个相关问题,至少在分析区域内,这对于更充分地估计降雨是一个重要问题。

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