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Diurnal Characteristics of Rainfall over the Contiguous United States and Northern Mexico in the Dynamically Downscaled Reanalysis Dataset (US10)

机译:在动态缩小的再分析数据集(US10)中,美国和墨西哥北部连续地区的降雨量的昼夜特征

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摘要

The diurnal characteristics of summer rainfall in the contiguous United States and northern Mexico were examined with the United States reanalysis for 5 years in 10-km horizontal resolution (US10), which is dynamically downscaled from the National Centers for Environmental Prediction National Center for Atmospheric Research (NCEP-NCAR) Global Reanalysis 1 using the Regional Spectral Model (RSM). The hourly precipitation outputs demonstrate a realistic structure in the temporal evolution of the observed rainfall episodes and their magnitudes across the United States without any prescriptions of the observed rainfall to the global reanalysis and the downscaled regional reanalysis. Nighttime rainfall over the Great Plains associated with eastward-propagating, mesoscale convective systems originating from the Rocky Mountains is also represented realistically in US 10, while the original reanalysis and most general circulation models (GCMs) have difficulties in capturing the series of nocturnal precipitation events in summer over the Plains. The results suggest an important role of the horizontal resolution of the model in resolving small-scale, propagating convective systems to improve the diurnal cycle of summer rainfall.
机译:美国连续10年的水平分辨率(US10)对美国连续5年进行了5年的再分析,研究了美国和墨西哥北部连续地区夏季降水的日变化特征,该分辨率是根据国家环境预测中心的动态降级的。 (NCEP-NCAR)使用区域光谱模型(RSM)的全球再分析1。每小时的降水量输出在整个美国观测到的降雨事件的时间演变及其量值中显示出一种现实的结构,而没有对全球再分析和缩减的区域再分析进行任何观测降雨的规定。在美国10年中,大平原上的夜间降雨与源自洛矶山脉的向东传播的中尺度对流系统相关,在美国10中也得到了实际体现,而原始的重新分析和大多数常规环流模型(GCM)难以捕获一系列夜间降水事件夏天在平原上。结果表明,该模型的水平分辨率在解决小规模传播对流系统以改善夏季降水的日循环方面具有重要作用。

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