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contributor authorLewandowski, Piotr A.
contributor authorEichinger, William E.
contributor authorKruger, Anton
contributor authorKrajewski, Witold F.
date accessioned2017-06-09T16:25:38Z
date available2017-06-09T16:25:38Z
date copyright2009/03/01
date issued2009
identifier issn0739-0572
identifier otherams-67668.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4209140
description abstractA significant scale gap between radar and in situ measurements of rainfall using rain gauges and disdrometers indicates a pressing need for improved knowledge of rainfall variability at the spatial scales below those of today?s operational radar rainfall products, that is, ?1?4 km. Lidar technology has the potential to fulfill this need, but there has been inconsistency in the literature pertaining to quantitative observations of rain using lidar. Several publications have stated that light scattering properties of raindrops could not be correlated with rain rates, while other papers have demonstrated the existence of such relationships. This note provides empirical evidence in support of the latter claim. The authors conducted a simple experiment using a near-horizontal-pointing elastic lidar to observe rain in Iowa City, Iowa, in the fall of 2005. The lidar signal was used to estimate rainfall quantities that were subsequently compared with independent estimates of the same quantities obtained from an optical disdrometer that was placed about 370 m from the lidar, ?10 m below the lidar beam. To perform the conversion from the raw lidar signal, the authors used an optical geometry-based procedure to estimate optical extinction data. A theoretical relationship between extinction coefficients and rain rates was derived based on a theoretical drop size distribution. The parameters of the relationship were found through a best-fit procedure using lidar and disdrometer data. The results show that the lidar-derived rain rates correspond to those obtained from the optical disdrometer with a root-mean-square difference of 55%. The authors conclude that although a great deal remains to be done to improve the inversion algorithm, lidar measurements of rain are possible and warrant further studies. Lidars deployed in conjunction with disdrometers can provide high spatial (<5 m) and temporal (<1 min disdrometer, ?1 s lidar) resolution data over a relatively long distance for rainfall measurements (1?2 km in the case of the University of Iowa lidar).
publisherAmerican Meteorological Society
titleLidar-Based Estimation of Small-Scale Rainfall: Empirical Evidence
typeJournal Paper
journal volume26
journal issue3
journal titleJournal of Atmospheric and Oceanic Technology
identifier doi10.1175/2008JTECHA1122.1
journal fristpage656
journal lastpage664
treeJournal of Atmospheric and Oceanic Technology:;2009:;volume( 026 ):;issue: 003
contenttypeFulltext


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