Evaluation of Spatial Errors of Precipitation Rates and Types from TRMM Spaceborne Radar over the Southern CONUS

被引:25
作者
Chen, S. [1 ,2 ]
Kirstetter, P. E. [1 ,2 ,3 ]
Hong, Y. [1 ,2 ]
Gourley, J. J. [3 ]
Tian, Y. D. [4 ,5 ]
Qi, Y. C. [3 ,6 ]
Cao, Q. [1 ,2 ]
Zhang, J. [3 ]
Howard, K. [3 ]
Hu, J. J. [7 ]
Xue, X. W. [1 ,2 ]
机构
[1] Univ Oklahoma, Sch Civil Engn & Environm Sci, Norman, OK 73019 USA
[2] Natl Weather Ctr, Adv Radar Res Ctr, Norman, OK 73072 USA
[3] NOAA, Natl Severe Storms Lab, Norman, OK 73069 USA
[4] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA
[5] NASA, Goddard Space Flight Ctr, Hydrol Sci Lab, Greenbelt, MD 20771 USA
[6] Univ Oklahoma, Cooperat Inst Mesoscale Meteorol Studies, Norman, OK 73019 USA
[7] Univ Oklahoma, Sch Comp Sci, Norman, OK 73019 USA
关键词
Precipitation; Atmosphere-land interaction; Hydrometeorology; RAIN PROFILING ALGORITHM; HYDROLOGICAL MODEL; GROUND VALIDATION; SYSTEM; QPE;
D O I
10.1175/JHM-D-13-027.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
In this paper, the authors estimate the uncertainty of the rainfall products from NASA and Japan Aerospace Exploration Agency's (JAXA) Tropical Rainfall Measurement Mission (TRMM) Precipitation Radar (PR) so that they may be used in a quantitative manner for applications like hydrologic modeling or merging with other rainfall products. The spatial error structure of TRMM PR surface rain rates and types was systematically studied by comparing them with NOAA/National Severe Storms Laboratory's (NSSL) next generation, high-resolution (1 km/5 min) National Mosaic and Multi-Sensor Quantitative Precipitation Estimation (QPE; NMQ/Q2) over the TRMM-covered continental United States (CONUS). Data pairs are first matched at the PR footprint scale (5 km/instantaneous) and then grouped into 0.25 degrees grid cells to yield spatially distributed error maps and statistics using data from December 2009 through November 2010. Careful quality control steps (including bias correction with rain gauges and quality filtering) are applied to the ground radar measurements prior to considering them as reference data. The results show that PR captures well the spatial pattern of total rainfall amounts with a high correlation coefficient (CC; 0.91) with Q2, but this decreases to 0.56 for instantaneous rain rates. In terms of precipitation types, Q2 and PR convective echoes are spatially correlated with a CC of 0.63. Despite this correlation, PR's total annual precipitation from convection is 48.82% less than that by Q2, which points to potential issues in the PR algorithm's attenuation correction, nonuniform beam filling, and/or reflectivity-to-rainfall relation. Finally, the spatial analysis identifies regime-dependent errors, in particular in the mountainous west. It is likely that the surface reference technique is triggered over complex terrain, resulting in high-amplitude biases.
引用
收藏
页码:1884 / 1896
页数:13
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