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dc.contributor.authorBoucher, Roland J.
dc.contributor.authorWieler, James G.
dc.date.accessioned2017-06-09T14:00:28Z
dc.date.available2017-06-09T14:00:28Z
dc.date.copyright1985/01/01
dc.date.issued1985
dc.identifier.issn0733-3021
dc.identifier.otherams-10806.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145964
dc.description.abstractA unique method that provides for relating radar-measured reflectivity factors to snowfall rates at the ground is presented. Data were provided by a CPS-9, 3.2 cm radar from six 1978 Massachusetts snowstorms A best-fit power-law relationship between hourly-averaged snowfall rate (depth) and radar reflectivity factor is determined. This derived relationship is found to be Z = 5.07S1.65 with a correlation coefficient of 0.91. With this relationship hourly snowfall rates are found to be accurate to within +41 to ?29% and total storm snowfall accumulation to within +44 to ?31%.
dc.publisherAmerican Meteorological Society
dc.titleRadar Determination of Snowfall Rate and Accumulation
dc.typeJournal Paper
dc.journal.volume24
dc.journal.issue1
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1985)024<0068:RDOSRA>2.0.CO;2
dc.journal.fristpage68
dc.journal.lastpage73
dc.treeJournal of Climate and Applied Meteorology:;1985:;volume( 024 ):;issue: 001
dc.contenttypeFulltext


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