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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Evaluation of the added value of a high-resolution regional climate model simulation of the South Asian summer monsoon climatology
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Evaluation of the added value of a high-resolution regional climate model simulation of the South Asian summer monsoon climatology

机译:评估南亚夏季季风气候学高分辨率区域气候模型模拟的附加值

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摘要

The South Asian summer monsoon (SASM) is a continental scale weather phenomenon, which fluctuates at a range of temporal and spatial scales. Although majority of global climate models are broadly able to simulate the large scale characteristics of the SASM, they generally have major deficiencies such as constraints in reproducing observed mean precipitation. It is generally anticipated that higher resolution regional climate models (RCMs) would be able to simulate an improved mean state owing to their capacity to better simulate fine temporal and spatial scale features and variability. Here, we analyse SASM simulations using a contemporary Hadley Centre RCM, forced by ERA-Interim reanalysis and observed sea surface temperature, at medium (0.44 degrees) and high (0.11 degrees) horizontal resolutions. Evaluation of the results show that, compared to the medium resolution RCM, the high resolution RCM is able to better resolve the interaction of the low level monsoon flow with the Himalayan orography leading to added value in simulating many aspects of SASM precipitation such as the seasonal mean, relative frequency distribution of daily precipitation, and various metrics of precipitation extremes. In contrast to many previous studies, maximum added value is note along the Indo-Gangetic plain rather than over the complex Himalayas, and the added values of up to 5 mm day(-1) and 50 days are noted for mean precipitation and number of wet days, respectively over the region. Similarly, added values of up to 15 and 3 mm day(-1) are noted for 95th percentile of daily precipitation and simple daily intensity index, respectively over central India and the Himalayan range. These results suggest that higher resolution RCMs have the potential to add more value when downscaling global climate model climate change projections.
机译:南亚夏季季风(SASM)是一个大陆尺度天气现象,其在一系列的时间和空间尺度上波动。虽然大多数全球气候模型广泛地能够模拟痉挛的大规模特征,但它们通常具有重大缺陷,例如再现观察到的平均沉淀的约束。通常预期,由于其能够更好地模拟精细的时间和空间尺度特征和可变性,因此预期更高的分辨率区域气候模型(RCMS)将能够模拟改进的平均状态。在这里,我们使用当代Hadley中心RCM分析SASM模拟,通过ERA-Instim Reany分析和观察海表面温度,在培养基(0.44度)和高(0.11度)的水平分辨率下进行海面温度。结果评价结果表明,与媒体分辨率RCM相比,高分辨率RCM能够更好地解决低水平季风流动与喜马拉雅人群的相互作用,从而在模拟季节性沉淀等许多方面的增加的额外值。平均,日降水的相对频率分布,以及沉淀极端的各种度量。与此以前的许多研究相比,最大附加值是沿着印度难看的平原而不是复杂的喜马拉雅山脉,并且最多5毫米日(-1)和50天的增加值对于平均降水和数量潮湿的日子,分别在该地区。类似地,最多15至3mm天(-1)的附加值分别在印度中部和喜马拉雅大范围内分别为95百分点的日降水和简单的日常强度指数。这些结果表明,在缩小全球气候模型气候变化预测时,更高的分辨率RCM可能会增加更多价值。

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