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contributor authorWalker, B.
contributor authorLamberth, L. S.
contributor authorStephens, J. J.
date accessioned2017-06-09T16:37:09Z
date available2017-06-09T16:37:09Z
date copyright1964/08/01
date issued1964
identifier issn0021-8952
identifier otherams-7104.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4212890
description abstractAn equal volume, dual-frequency radar system is used to obtain a quantitative characterization of a precipitation volume. The power back-scattered is related to the rainfall rate through the use of an assumed exponential drop-size distribution and the Mie radar cross section. A method is given whereby the relative consistency of a dual-frequency radar system is aided by calibration in the Rayleigh scattering region of a light rainshower. Discrepancies that occur in the observed rainfall rate are attributed to: 1) errors in the form of the assumed drop-size distribution, and 2) local vertical velocity and velocity divergence. Simultaneous observations of precipitation by the dual-frequency radar and raingages are shown for two rain situations.
publisherAmerican Meteorological Society
titleDual-Frequency Radar Observations of Precipitation
typeJournal Paper
journal volume3
journal issue4
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1964)003<0430:DFROOP>2.0.CO;2
journal fristpage430
journal lastpage438
treeJournal of Applied Meteorology:;1964:;volume( 003 ):;issue: 004
contenttypeFulltext


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