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Global-scale evaluation of 22 precipitation datasets using gauge observations and hydrological modeling

机译:使用量表观测和水文模型对22个降水数据集进行全球规模评估

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We undertook a comprehensive evaluation of 22 gridded (quasi-)global (sub-)daily precipitation (iP/i) datasets for the period 2000–2016. Thirteen non-gauge-corrected iP/i datasets were evaluated using daily iP/i gauge observations from 76?086 gauges worldwide. Another nine gauge-corrected datasets were evaluated using hydrological modeling, by calibrating the HBV conceptual model against streamflow records for each of 9053 small to medium-sized (?&??50?000?kmsup2/sup) catchments worldwide, and comparing the resulting performance. Marked differences in spatio-temporal patterns and accuracy were found among the datasets. Among the uncorrected iP/i datasets, the satellite- and reanalysis-based MSWEP-ng?V1.2 and?V2.0 datasets generally showed the best temporal correlations with the gauge observations, followed by the reanalyses (ERA-Interim, JRA-55, and NCEP-CFSR) and the satellite- and reanalysis-based CHIRP?V2.0 dataset, the estimates based primarily on passive microwave remote sensing of rainfall (CMORPH?V1.0, GSMaP?V5/6, and TMPA 3B42RT?V7) or near-surface soil moisture (SM2RAIN-ASCAT), and finally, estimates based primarily on thermal infrared imagery (GridSat?V1.0, PERSIANN, and PERSIANN-CCS). Two of the three reanalyses (ERA-Interim and JRA-55) unexpectedly obtained lower trend errors than the satellite datasets. Among the corrected iP/i datasets, the ones directly incorporating daily gauge data (CPC Unified, and MSWEP?V1.2 and?V2.0) generally provided the best calibration scores, although the good performance of the fully gauge-based CPC Unified is unlikely to translate to sparsely or ungauged regions. Next best results were obtained with iP/i estimates directly incorporating temporally coarser gauge data (CHIRPS?V2.0, GPCP-1DD?V1.2, TMPA 3B42?V7, and WFDEI-CRU), which in turn outperformed the one indirectly incorporating gauge data through another multi-source dataset (PERSIANN-CDR V1R1). Our results highlight large differences in estimation accuracy, and hence the importance of iP/i dataset selection in both research and operational applications. The good performance of MSWEP emphasizes that careful data merging can exploit the complementary strengths of gauge-, satellite-, and reanalysis-based iP/i estimates.
机译:我们对2000-2016年期间的22个网格化(准)全球(次)日降水量( P )数据集进行了全面评估。使用来自全球76?086个量具的每日 P 量具观测值,评估了13个未经量具校正的 P 数据集。通过对9053个中小型(?<?50?000?km 2 )中的每一个记录的流量记录校准HBV概念模型,使用水文模型评估了另外9个校正量表的数据集。全球范围内的流域,并比较结果。在数据集中发现时空模式和准确性存在明显差异。在未校正的 P 数据集中,基于卫星和重新分析的MSWEP-ng?V1.2和?V2.0数据集通常与量具观测值表现出最佳的时间相关性,然后进行重新分析(ERA -临时,JRA-55和NCEP-CFSR)以及基于卫星和再分析的CHIRP?V2.0数据集,这些估算主要基于无源微波降雨遥感(CMORPH?V1.0,GSMaP?V5 / 6) ,以及TMPA 3B42RT?V7)或近地表土壤湿度(SM2RAIN-ASCAT),最后,估计主要基于热红外图像(GridSat?V1.0,PERSIANN和PERSIANN-CCS)。三个重新分析中的两个(ERA-Interim和JRA-55)意外地获得了比卫星数据集更低的趋势误差。在校正后的 P 数据集中,直接使用每日量表数据(CPC Unified和MSWEP?V1.2和?V2.0)的数据通常提供最佳的校准分数,尽管完全基于规范的CPC Unified不太可能转换为稀疏或未开放的区域。使用 P 估计直接获得时间上较粗的轨距数据(CHIRPS?V2.0,GPCP-1DD?V1.2,TMPA 3B42?V7和WFDEI-CRU)可获得次佳结果。胜过通过另一个多源数据集(PERSIANN-CDR V1R1)间接包含量规数据的数据。我们的结果突显了估计准确性方面的巨大差异,因此 P 数据集选择在研究和运营应用中的重要性。 MSWEP的良好性能强调了仔细的数据合并可以利用基于量具,卫星和基于再分析的 P 估计的互补优势。

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