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Interannual and low-frequency variability of Upper Indus Basin winter/spring precipitation in observations and CMIP5 models

机译:观测值和CMIP5模型的上印度河流域冬/春季降水的年际和低频变化

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An assessment is made of the ability of general circulation models in the CMIP5 ensemble to reproduce observed modes of low-frequency winter/spring precipitation variability in the region of the Upper Indus basin (UIB) in south-central Asia. This season accounts for about two thirds of annual precipitation totals in the UIB and is characterized by "western disturbances" propagating along the eastward extension of the Mediterranean storm track. Observational data are utilized for for spatiotemporal characterization of the precipitation seasonal cycle, to compute seasonalized spectra and finally, to examine teleconnections, in terms of large-scale patterns in sea-surface temperature (SST) and atmospheric circulation. Annual and lowpassed variations are found to be associated primarily with SST modes in the tropical and extratropical Pacific. A more obscure link to North Atlantic SST, possibly related to the North Atlantic Oscillation, is also noted. An ensemble of 31 CMIP5 models is then similarly assessed, using unforced preindustrial multi-century control runs. Of these models, eight are found to reproduce well the two leading modes of the observed seasonal cycle. This model subset is then assessed in the spectral domain and with respect to teleconnection patterns, where a range of behaviors is noted. Two model families each account for three members of this subset. The degree of within-family similarity in behavior is shown to reflect underlying model differences. The results provide estimates of unforced regional hydroclimate variability over the UIB on interannual and decadal scales and the corresponding far-field influences, and are of potential relevance for the estimation of uncertainties in future water availability.
机译:评估了CMIP5集合中的一般环流模型的能力,以重现亚洲中南部上印度河流域(UIB)地区低频冬季/春季降水变化的观测模式。该季节约占UIB年降水总量的三分之二,其特征是沿着地中海风暴径的东延传播的“西部扰动”。观测数据可用于降水季节周期的时空特征,计算季节频谱以及最后检查海面温度(SST)和大气环流的大规模模式的遥相关。发现年和低通变化主要与热带和温带太平洋的海表温度模式有关。还注意到与北大西洋SST的联系更加模糊,可能与北大西洋涛动有关。然后使用非强制性的工业化多世纪控制运行对31个CMIP5模型的集合进行类似的评估。在这些模型中,发现有八种可以很好地再现观察到的季节性周期的两种主导模式。然后在频谱域中并根据远程连接模式评估该模型子集,其中记录了一系列行为。两个模型族各自占该子集的三个成员。行为上家庭内部相似度显示出潜在的模型差异。结果提供了在年际和年代际尺度上UIB非强迫区域水气候变化的估计以及相应的远场影响,并且对于估计未来水的不确定性具有潜在的相关性。

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