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首页> 外文期刊>Journal of hydrometeorology >Reprocessed, Bias-Corrected CMORPH Global High-Resolution Precipitation Estimates from 1998
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Reprocessed, Bias-Corrected CMORPH Global High-Resolution Precipitation Estimates from 1998

机译:重新加工,偏置偏置CMORPH全球高分辨率降水估算从1998年

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The Climate Prediction Center (CPC) morphing technique (CMORPH) satellite precipitation estimates are reprocessed and bias corrected on an 8 km 3 8 km grid over the globe (608S-608N) and in a 30-min temporal resolution for an 18-yr period from January 1998 to the present to form a climate data record (CDR) of high-resolution global precipitation analysis. First, the purely satellite-basedCMORPH precipitation estimates (raw CMORPH) are reprocessed. The integration algorithmis fixed and the input level 2 passivemicrowave (PMW) retrievals of instantaneous precipitation rates are from identical versions throughout the entire data period. Bias correction is then performed for the raw CMORPH through probability density function (PDF) matching against the CPC daily gauge analysis over land and through adjustment against the Global Precipitation Climatology Project (GPCP) pentad merged analysis of precipitation over ocean. The reprocessed, bias-corrected CMORPH exhibits improved performance in representing the magnitude, spatial distribution patterns, and temporal variations of precipitation over the global domain from 60 degrees S to 60 degrees N. Bias in the CMORPH satellite precipitation estimates is almost completely removed over land during warm seasons (May-September), while during cold seasons (October-April) CMORPH tends to underestimate the precipitation due to the less-thandesirable performance of the current-generation PMW retrievals in detecting and quantifying snowfall and cold season rainfall. An intercomparison study indicated that the reprocessed, bias-corrected CMORPH exhibits consistently superior performance than the widely used TRMM 3B42 (TMPA) in representing both daily and 3-hourly precipitation over the contiguous United States and other global regions.
机译:气候预测中心(CMORPH)的变形技术(CMORPH)卫星降水估算重新加工,并在全球(608S-608N)上8km 3 8km网格上校正偏差,并以18年的时间为单位的30分钟的时间分辨率从1998年1月到现在,形成高分辨率全球降水分析的气候数据记录(CDR)。首先,重新加工纯粹的卫星基于卫星沉淀估计(原料Cmorph)。整合算法固定和输入级别2 Passivemroveave(PMW)瞬时降水率的检索来自整个数据周期的相同版本。然后通过概率密度函数(PDF)对诸如土地的CPC每日仪表分析的概率密度函数(PDF)进行偏压校正,并通过对全球降水的调整(GPCP)PENTAD对海洋降水分析的调整。再加工的偏见校正的Cmorph表现出改进的性能,在表示从60摄氏度到60度的全局领域的降水的时间变化和时间变化。在CMORPH卫星降水估计中的偏差几乎完全消除在陆地上在温暖的季节(5月至9月)期间,虽然在冷季节(4月至4月)CMORPH期间,由于当前发电的PMW检测和量化降雪和寒冷的季节降雨而导致的降水趋于低估降水。依比鉴定研究表明,再加工的偏置校正的CMORPH表现出比广泛使用的TRMM 3B42(TMPA)在连续的美国和其他全球区域上的每日和3小时降水中的广泛使用的TRMM 3B42(TMPA)呈始终如一的优异性能。

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