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dc.contributor.authorTuttle, John D.
dc.contributor.authorRinehart, Ronald E.
dc.date.accessioned2017-06-09T13:59:51Z
dc.date.available2017-06-09T13:59:51Z
dc.date.copyright1983/11/01
dc.date.issued1983
dc.identifier.issn0733-3021
dc.identifier.otherams-10612.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145749
dc.description.abstractIn using a dual-wavelength radar system to detect hail, erroneous positive hail signals can result because of the stronger attenuation of the shorter wavelength radar beam. We present a simple technique to correct for attenuation in dual-wavelength analyses. The technique makes use of an attenuation-reflectivity relationship of the form, A = CZxp, where Zx is the S-band reflectivity, C is a coefficient which is determined on a ray-by-ray basis, and p is the exponent, which is assumed to be a constant. In situations where rays of radar data contain a mixture of rain and hail, the attenuation-correction scheme can erroneously apportion more of the attenuation to hail regions rather than to rain regions. The scheme is modified to account for such situations.
dc.publisherAmerican Meteorological Society
dc.titleAttenuation Correction in Dual-Wavelength Analyses
dc.typeJournal Paper
dc.journal.volume22
dc.journal.issue11
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1983)022<1914:ACIDWA>2.0.CO;2
dc.journal.fristpage1914
dc.journal.lastpage1921
dc.treeJournal of Climate and Applied Meteorology:;1983:;volume( 022 ):;issue: 011
dc.contenttypeFulltext


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