@@ 1. Introduction Accurate estimates ofprecipitation at both high temporal and spatial resolutions are required fo r m any ap plications. W hereas rain g auge d ata ar e routinely av ailable, they are sparse in many important regions even over land. Many gauge stations report only 6 hourly or even da ily r ainfall amounts. The w eather r adar ne twork c ould pr ovide g ood s patial and temporal co verage, b ut p roblems asso ciated w ith inter-radar c alibration a nd b Iockage by mountains still I imit i ts a ccuracy a nd c apability. R etrievals o f p recipitation from s atellite measurements be comet hem ajorp roductsw idely us edt odoc ument precipitation characteristics and verification of model predictions/simulations.
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机译：@@ 1.简介精确的估计在任何AP折叠中都需要高时和空间分辨率的折叠。 Whereas rain g auge d ata ar e arecely av a av，它们在许多重要地区都稀疏，即使在土地上也是如此。许多规格站仅报告每小时6小时甚至是Da Ily r Ainfall金额。 w eather r adar ne twork c oould pr ovide g ood s露天和颞co reserage，b ut p rooblems comate inter-radar c aligation a nd b iockage by山脉仍然是我认为一个ccuracy a nd c appable 。来自Satellite测量的re etrievals of p核算是Comet下摆Ajorp roductsWeary美国EDT Odoc Ument降水特性和模型预测/模拟的验证。
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