A geostatistical method for Texas NexRad data calibration

Rainfall is one of the most important hydrologic model inputs and is recognized as a random process in time and space. Rain gauges generally provide good quality data, however they are usually too sparse to capture the spatial variability. Radar estimates provide a better spatial representation of r...

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Bibliographic Details
Published inEnvironmetrics (London, Ont.) Vol. 19; no. 1; pp. 1 - 19
Main Authors Li, Bo, Eriksson, Marian, Srinivasan, Raghavan, Sherman, Michael
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 01.02.2008
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Summary:Rainfall is one of the most important hydrologic model inputs and is recognized as a random process in time and space. Rain gauges generally provide good quality data, however they are usually too sparse to capture the spatial variability. Radar estimates provide a better spatial representation of rainfall patterns, but they are subject to substantial biases. Our calibration of radar estimates using gauge data takes season, rainfall type, and rainfall amount into account, and is accomplished via a combination of threshold estimation, bias reduction, regression techniques, and geostatistical procedures. We explore the varying‐coefficient model to adapt to the temporal variability of rainfall. The methods are illustrated using Texas rainfall data in 2003, which includes Weather Surveillance Radar‐1988 Doppler (WSR‐88D) radar‐reflectivity data and the corresponding rain gauge measurements. Simulation experiments are carried out to evaluate the accuracy of our methodology. Copyright © 2007 John Wiley & Sons, Ltd.
Bibliography:istex:60AC01DD45422E705C13FEF7BF08F70E5364B99D
ark:/67375/WNG-73MNZ7MX-V
ArticleID:ENV848
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:1180-4009
1099-095X
DOI:10.1002/env.848