Evaluation of Spatial Errors of Precipitation Rates and Types from TRMM Spaceborne Radar over the Southern CONUSSource: Journal of Hydrometeorology:;2013:;Volume( 014 ):;issue: 006::page 1884Author:Chen, S.
,
Kirstetter, P. E.
,
Hong, Y.
,
Gourley, J. J.
,
Tian, Y. D.
,
Qi, Y. C.
,
Cao, Q.
,
Zhang, J.
,
Howard, K.
,
Hu, J. J.
,
Xue, X. W.
DOI: 10.1175/JHM-D-13-027.1Publisher: American Meteorological Society
Abstract: n 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° 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.
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contributor author | Chen, S. | |
contributor author | Kirstetter, P. E. | |
contributor author | Hong, Y. | |
contributor author | Gourley, J. J. | |
contributor author | Tian, Y. D. | |
contributor author | Qi, Y. C. | |
contributor author | Cao, Q. | |
contributor author | Zhang, J. | |
contributor author | Howard, K. | |
contributor author | Hu, J. J. | |
contributor author | Xue, X. W. | |
date accessioned | 2017-06-09T17:15:35Z | |
date available | 2017-06-09T17:15:35Z | |
date copyright | 2013/12/01 | |
date issued | 2013 | |
identifier issn | 1525-755X | |
identifier other | ams-81991.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4225054 | |
description abstract | n 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° 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. | |
publisher | American Meteorological Society | |
title | Evaluation of Spatial Errors of Precipitation Rates and Types from TRMM Spaceborne Radar over the Southern CONUS | |
type | Journal Paper | |
journal volume | 14 | |
journal issue | 6 | |
journal title | Journal of Hydrometeorology | |
identifier doi | 10.1175/JHM-D-13-027.1 | |
journal fristpage | 1884 | |
journal lastpage | 1896 | |
tree | Journal of Hydrometeorology:;2013:;Volume( 014 ):;issue: 006 | |
contenttype | Fulltext |