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Evaluation of precipitation estimates over CONUS derived from satellite, radar, and rain gauge data sets at daily to annual scales (2002–2012)

机译:从卫星,雷达和雨量计数据集得出的CONUS降水估值的评估,每日至年度尺度(2002-2012年)

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We use a suite of quantitative precipitation estimates (QPEs) derived from satellite, radar, and surface observations to derive precipitation characteristics over the contiguous United States (CONUS) for the period 2002–2012. This comparison effort includes satellite multi-sensor data sets (bias-adjusted TMPA 3B42, near-real-time 3B42RT), radar estimates (NCEP Stage IV), and rain gauge observations. Remotely sensed precipitation data sets are compared with surface observations from the Global Historical Climatology Network-Daily (GHCN-D) and from the PRISM (Parameter-elevation Regressions on Independent Slopes Model). The comparisons are performed at the annual, seasonal, and daily scales over the River Forecast Centers (RFCs) for CONUS. Annual average rain rates present a satisfying agreement with GHCN-D for all products over CONUS (±6%). However, differences at the RFC are more important in particular for near-real-time 3B42RT precipitation estimates (?33 to +49%). At annual and seasonal scales, the bias-adjusted 3B42 presented important improvement when compared to its near-real-time counterpart 3B42RT. However, large biases remained for 3B42 over the western USA for higher average accumulation (≥ 5 mm daysup?1/sup) with respect to GHCN-D surface observations. At the daily scale, 3B42RT performed poorly in capturing extreme daily precipitation ( 4 in. daysup?1/sup) over the Pacific Northwest. Furthermore, the conditional analysis and a contingency analysis conducted illustrated the challenge in retrieving extreme precipitation from remote sensing estimates.
机译:我们使用从卫星,雷达和地表观测获得的一套定量降水估算(QPE),得出2002-2012年间美国连续(CONUS)的降水特征。这项比较工作包括卫星多传感器数据集(经偏置调整的TMPA 3B42,近实时3B42RT),雷达估计(NCEP第四阶段)和雨量计观测值。将遥感的降水数据集与每日全球历史气候学网络(GHCN-D)和PRISM(独立斜坡模型的参数高程回归)的地面观测结果进行比较。比较是在CONUS的河流预报中心(RFC)上按年度,季节和每日规模进行的。年平均降雨率与GHCN-D达成了对CONUS(±6%)以上所有产品的令人满意的协议。但是,RFC的差异更为重要,特别是对于近实时3B42RT降水估计(33%至+ 49%)。在年度和季节尺度上,与近实时的3B42RT相比,经过偏差调整的3B42表现出重要的改进。但是,相对于GHCN-D表面观测,美国西部3B42仍存在较大偏差,以实现更高的平均积累量(≥5 mm day ?1 )。在每日尺度上,3B42RT在捕获西北太平洋上的极端每日降水(> 4 in。day ?1 )方面表现不佳。此外,进行的条件分析和偶发性分析说明了从遥感估算中检索极端降水的挑战。

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