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EVALUATION OF HIGH-RESOLUTION SATELLITE RAINFALL DATA OVER SINGAPORE

机译:新加坡高分辨率卫星降雨数据评估

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The uncertainties of two high-resolution satellite precipitation products (TRMM 3B42 v7.0 and GSMaP v5.222) were investigated by comparing them against rain gauge observations in Singapore on sub-daily scales. The satellite-borne precipitation products are assessed in terms of diurnal cycle and extreme precipitation for 10 years from Dec. 2000 to Nov. 2010. The satellite products agree well on the late afternoon maximum and heavier rainfall of gauge-based data in winter season when the ITCZ is located in Singapore. However, they fail in estimating diurnal cycle in summer. The disagreement in summer can be accounted for by the dominant satellite overpass time (about 14:00 SGT) later than the diurnal peak time (about 09:00 SGT) of gauge precipitation. According to analysis of extreme precipitation indices, both satellite datasets tend to overestimate the light rain and frequency but underestimate high intensity precipitation and the length of dry spell over all stations. In particular, the uncertainty of extreme precipitation is higher in GSMaP than in TRMM, possibly due to the several effects such as satellite merging algorithm, the finer spatio-temporal scale of high intensity precipitation, and swath time of satellite. Such discrepancies between satellite-born and gauge-based precipitations at sub-daily scale can possibly lead to distorting analysis of precipitation characteristics and/or application model results, this research on quantification of their uncertainty is useful in many respects, especially that the satellite products can stand scrutiny overplaces/stations where there are no good data to be compared against.
机译:通过将它们与新加坡的雨量测量观测相比,研究了两种高分辨率卫星沉淀产品的不确定性(TRMM 3B42 V7.0和GSMAP v5.222)对新加坡的雨量尺寸观察。星载降水产品在昼夜周期和极端降水为10年来评估从2000年12月至2010年十一月卫星产品在下午晚些时候最大和更重的降雨基于计数据的吻合在冬季时热带辐合带位于新加坡。然而,他们在夏季估算昼夜周期。夏季的分歧可以由优势卫星立即时间(约14:00)之后的差价峰值时间(约09:00 SGT)占据尺寸沉淀。根据极端降水指数的分析,卫星数据集两种数据集往往估计轻雨和频率,而是低于所有站点的高强度降水量和干法施加的长度。特别是,GSMap的极端沉淀的不确定度高于TRMM,可能是由于诸如卫星合并算法的若干效果,高强度沉淀的更精细的时空规模和卫星的SWAP时间。卫星出生和仪表的沉淀在亚日规模之间的差异可能导致降水特性和/或应用模型结果的扭曲分析,这对其不确定性的量化的研究在许多方面都很有用,特别是卫星产品可以在没有良好数据的情况下突击审查过度空间/站。

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