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Quantitative estimation of orographic precipitation over the Himalayas by using TRMM/PR and a dense network of rain gauges

机译:利用TRMM / PR和密集的雨量计网络对喜马拉雅山地形降水进行定量估计

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The Precipitation Radar (PR) data acquired by the Tropical Rainfall Measuring Mission (TRMM) over its 10 years of observation can be used to show the monthly rainfall patterns over the Himalayas. To validate and adjust these patterns, we used a dense network of rain gauges to measure daily precipitation over Nepal, Bangladesh, Bhutan, Pakistan, India, Myanmar, and China. We then compared TRMM/PR and rain gauge data in 0.05-degree grid cells (an approximately 5.5-km mesh). Compared to the rain gauge observations, PR systematically underestimated precipitation by 28% to 38% in summer (July-September). Monthly PR climatology was adjusted based on the monthly regressions between the 2 sets of data, and depicted.
机译:热带降雨测量团(TRMM)在其10年的观测中获得的降水雷达(PR)数据可用于显示喜马拉雅山脉的每月降雨模式。为了验证和调整这些模式,我们使用了密集的雨量计网络来测量尼泊尔,孟加拉国,不丹,巴基斯坦,印度,缅甸和中国的日降水量。然后,我们在0.05度网格(约5.5公里网格)中比较了TRMM / PR和雨量计数据。与降雨仪的观测结果相比,PR在夏季(7月至9月)系统地低估了28%至38%的降水量。基于两组数据之间的每月回归,对每月PR气候进行了调整,并进行了描述。

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