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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Assessing two different climatic models and the NCEP-NCAR reanalysis data for the description of winter precipitation in the Iberian Peninsula
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Assessing two different climatic models and the NCEP-NCAR reanalysis data for the description of winter precipitation in the Iberian Peninsula

机译:评估两种不同的气候模式和NCEP-NCAR再分析数据,以描述伊比利亚半岛的冬季降水

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摘要

The main questions motivating this study are: Can climate simulations describe the observations? To what extent can we use climate models to predict climate change? For this purpose, an analysis was made of the correspondences and/or discrepancies between observed winter precipitation data and the data from the National Centers for Environmental Prediction-National Center for Atmospheric Research (NCEP-NCAR) reanalysis project, and from two global climatic models: ECHAM4/OPYC3 and HadCM3. The data used correspond to the accumulated winter precipitation for the period 1949-2000, and comparisons of the mean and variability patterns were made. The methods used were principal components analysis, to break down variability and reduce the dimensions of the fields, and correlation and cross-spectrum analyses for comparison of the time series. For all these, we studied the suitability of their average distributions, as well as their modes of spatial and spectral variability. The results for the Iberian Peninsula show good agreement between the precipitation data of the NCEP-NCAR reanalysis and the observations, both in the average analysis and in the main modes of spatial and time variability. Therefore, the reanalysis data were proved to be a good resource for interpreting climate variations. As regards the climatic models considered, in general the results point to their suitability for describing the spatial distribution of winter precipitation, whereas the spectral association is less appropriate. The variability of the precipitation data was related to circulation patterns and teleconnection indices, such as the North Atlantic oscillation and the Arctic oscillation. The results allow us to conclude that the discrepancies between the two models and observations must be due to a weak representation of the interannual variability.
机译:推动这项研究的主要问题是:气候模拟能否描述观测结果?我们可以在多大程度上使用气候模型来预测气候变化?为此,对观测到的冬季降水数据与国家环境预测中心-国家大气研究中心(NCEP-NCAR)再分析项目以及两个全球气候模型的数据之间的对应关系和/或差异进行了分析。 :ECHAM4 / OPYC3和HadCM3。所使用的数据对应于1949-2000年期间的冬季累积降水量,并对均值和变异性模式进行了比较。所使用的方法是主成分分析(用于分解可变性并减小字段的维数),以及相关性和互谱分析以比较时间序列。对于所有这些,我们研究了它们平均分布的适用性,以及它们的空间和光谱可变性模式。伊比利亚半岛的结果表明,在平均分析以及空间和时间可变性的主要模式中,NCEP-NCAR再分析的降水数据与观测值之间具有良好的一致性。因此,再分析数据被证明是解释气候变化的良好资源。关于所考虑的气候模型,总体而言,结果表明它们适合描述冬季降水的空间分布,而光谱关联则不太合适。降水数据的变化与环流模式和遥相关指数有关,例如北大西洋振荡和北极振荡。结果使我们得出结论,两个模型和观测值之间的差异必须归因于年际变化的弱表示。

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