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contributor authorBerenguer, Marc
contributor authorZawadzki, Isztar
date accessioned2017-06-09T16:27:11Z
date available2017-06-09T16:27:11Z
date copyright2009/06/01
date issued2009
identifier issn0882-8156
identifier otherams-68113.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209636
description abstractThe contribution of various physical sources of uncertainty affecting radar rainfall estimates at the ground has been recently quantified at a resolution typically used in schemes assimilating rainfall at the ground onto mesoscale models. Here, the contribution of the two most important sources of uncertainty at nonattenuating wavelengths (the range-dependent error and the uncertainty due to the Z?R transformation) and their interaction are studied as a function of the resolution of radar observations. The analysis is carried out using a large dataset of collocated reflectivity profiles from the McGill S-band radar and disdrometric measurements obtained in stratiform rainfall at resolutions of 1 ? 1, 5 ? 5, and 15 ? 15 km2. Results show that the errors affecting radar quantitative precipitation estimation (QPE) have a strong dependence with range, and that their structure is scale dependent. At the analyzed resolutions, QPE errors are significantly correlated in time and over several grid points.
publisherAmerican Meteorological Society
titleA Study of the Error Covariance Matrix of Radar Rainfall Estimates in Stratiform Rain. Part II: Scale Dependence
typeJournal Paper
journal volume24
journal issue3
journal titleWeather and Forecasting
identifier doi10.1175/2008WAF2222210.1
journal fristpage800
journal lastpage811
treeWeather and Forecasting:;2009:;volume( 024 ):;issue: 003
contenttypeFulltext


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