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Multi-model climate projections of the main cyclogenesis hot-spots and associated winds over the eastern coast of South America

机译:主要环比的多模型气候预测热点和南美洲东部海岸的相关风

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In this study, multi-model ensembles are used to understand regional features of future climate trends of cyclones and associated winds in eastern South America. For this, we consider three cyclogenetic hot-spot regions located in south-southeastern Brazil, extreme southern Brazil-Uruguay, and southern Argentina, named, respectively, RG1, RG2 and RG3. The multi-model ensembles consist of four RegCM4 downscalings (RegCM4s) nested in three different global circulation models (GCMs) from CMIP5 under RCP8.5 for the period 1979-2100. ERA-Interim, and CFSR provide the reanalyses ensemble. For the present climate (1979-2005), RegCM4s and GCMs simulate the main characteristics of the cyclone's genesis and propagation. There is greater agreement between RegCM4s and reanalyses regarding the magnitude and location of stronger winds associated with intense cyclones starting in RG1 and RG2. An important added value is the greater ability of RegCM4s to capture the observed features (phase and amplitude of the annual cycle, intensity, and near surface winds) of cyclogenesis starting in regions away from the boundary domain, such as in RG1 and RG2. In these regions, RegCM4s present smaller (higher) error (correlation) for the frequency of cyclones than GCMs, which improves the representation of cyclones for the whole southwestern South Atlantic domain. RegCM4s are able to simulate in greater agreement with reanalysis than GCMs, the initially stronger cyclones and associated low level winds. For these intense cyclones in the future climate, an intensification of low-level winds off the coast (south-southeast Brazil and south Argentina) and a shift to the south of the upper-level polar jet are projected. Furthermore, there is a clear trend towards decrease in the number of cyclogeneses in each hot-spot region, indicating that each intense cyclone will be associated with stronger low level winds near the eastern South America coast at the end of the twenty-first century.
机译:在本研究中,多模型集合用于了解南美洲东部旋风和相关风的未来气候趋势的区域特征。为此,我们考虑了位于巴西南部的巴西,巴西 - 乌拉圭南部,阿根廷南部,分别为RG1,RG2和RG3的三个环素热点区域。多模型集合组成于1979-2100期间在RCP8.5下的CMIP5下的三种不同全局循环模型(GCMS)中嵌套的四个REGCM4缩小型(REGCM4S)。 ERA-ANTERIM,CFSR提供了Reanalyses Ensemble。对于目前的气候(1979-2005),REGCM4S和GCMS模拟了旋风的成因和繁殖的主要特征。 Regcm4s和Reanalyses之间的达成符合较大的关于与RG1和RG2开始的强风相关的更强风的幅度和位置。重要的附加值是REGCM4S在远离边界域的区域中捕获循环生成的观察到的特征(相循环,强度和近视,表面风的相位和近的表面风)的能力,例如RG1和RG2。在这些区域中,REGCM4S对旋风频率的频率较小(更高)误差(相关性),这提高了整个西南南大西洋领域的旋风的表示。 REGCM4S能够以比GCMS更大的重新分析进行模拟,最初更强大的旋风和相关的低水平风。对于未来的气候中的这些激烈的旋风,将沿着海岸(巴西和南阿根廷南部)的低级风的强化,并预计向上级极性喷气机南部的转变。此外,每个热点地区的环比导数量有明显的趋势,表明每个强烈的旋风器在二十一世纪末到东南美洲海岸附近的强大风电有关。

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