文章摘要
孙乐强,郝振纯,王加虎,Ioan Nistor,Ousmane Seidou.TMPA 卫星降水数据的评估与校正[J].水利学报,2014,45(10):
TMPA 卫星降水数据的评估与校正
Assessment and correction of TMPA products 3B42RT and 3B42V6
  
DOI:
中文关键词: 卫星降水  评估  校正  降水重心  水文模型
英文关键词: TMPA  assessment  correction  precipitation centroid  hydrological model
基金项目:
作者单位
孙乐强 1. 渥太华大学土木工程系渥太华K1N 6N5 加拿大2. 河海大学水文水资源与水利工程科学国家重点实验室江苏南京210098 
郝振纯 河海大学水文水资源与水利工程科学国家重点实验室江苏南京210098 
王加虎 河海大学水文水资源与水利工程科学国家重点实验室江苏南京210098 
Ioan Nistor 渥太华大学土木工程系渥太华K1N 6N5 加拿大 
Ousmane Seidou 渥太华大学土木工程系渥太华K1N 6N5 加拿大 
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中文摘要:
      卫星遥感降水由于时空分辨率的优势在现代水文模拟中正起着越来越大的作用。本研究对黄河源区的两套卫星降水产品(TMPA准实时3B42RT和研究数据3B42V6)进行了详细评估,结果表明,3B42RT与3B42V6相比会明显高估地面降水,而两者对降水事件的反演能力基本一致。通过引入“降水重心”的概念,两套卫星降水产品均可以基本反映降水的空间分布及长期演变过程。在两者尤其是3B42RT数据的校正中,首先将卫星数据与地面站点月降水对比,再等比例降尺度回日降水,然后尝试逐步订正和最优插值两种残差处理方法,从而使降水量和降水分布的精度进一步提高。最后用校正后的卫星降水驱动分布式水文模型,利用输出径流间接验证校正的效果。
英文摘要:
      The application of Satellite Remote Sensing precipitation has great potential in modern hydrology.In this paper, two sets of TMPA products: 3B42RT and 3B42V6 are evaluated and corrected in the area of the headwater region of the Yellow River. Although RT product highly overestimates real precipitation, it has similar accuracy as V6 when it comes to precipitation event prediction and precipitation spatial distribution. Both products are able to describe the spatial distribution of annual precipitation as well as the temporal and spatial change of areal precipitation with the help of the research on the newly introduced‘precipitation centroid’. In the correction of RT product, RT data is firstly compared to ground gauged precipitation on monthly basis and then downscaled to daily basis. The Successive Correction and Optimal Interpolation are applied for further handling of the residuals. Satisfying results are obtained from both methods. A simple distributed hydrological model is driven by the corrected RT products as well as uncorrected ones and ground gauged precipitation. The RT product which has advantage of ‘real time’ compared to V6,turns out to be satisfactory, if not better, to be used as model input for stream flow simulation after the correction.
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