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contributor authorShipley, S. T.
contributor authorEloranta, E. W.
contributor authorWeinman, J. A.
date accessioned2017-06-09T17:36:20Z
date available2017-06-09T17:36:20Z
date copyright1974/10/01
date issued1974
identifier issn0021-8952
identifier otherams-8795.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4231677
description abstractMonostatic lidar is explored as a means for determining the rainfall rate over an extended atmospheric path with a spatial resolution comparable to that of rain gages. An empirical relationship is established between the optical extinction coefficient of rain ?r (km?1) and the rainfall rate R (mm hr?1). Correlation of lidar-derived rainfall extinction and gage rainfall rates at Madison gives ?r = 0.16 R0.74. The ?r-R relations obtained from the work of other authors compare well with this relationship. A lidar equation which accounts for the multiple scattering of light in rain is presented. A numerical procedure which derives estimates of ?r as a function of range from lidar returns is developed. Examples of lidar-derived rainfall rate range profiles in spatially inhomogeneous thunderstorms are given.
publisherAmerican Meteorological Society
titleMeasurement of Rainfall Rates by Lidar
typeJournal Paper
journal volume13
journal issue7
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1974)013<0800:MORRBL>2.0.CO;2
journal fristpage800
journal lastpage807
treeJournal of Applied Meteorology:;1974:;volume( 013 ):;issue: 007
contenttypeFulltext


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