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dc.contributor.authorSchmid, W.
dc.contributor.authorWaldvogel, A.
dc.date.accessioned2017-06-09T14:01:16Z
dc.date.available2017-06-09T14:01:16Z
dc.date.copyright1986/07/01
dc.date.issued1986
dc.identifier.issn0733-3021
dc.identifier.otherams-11023.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146206
dc.description.abstractRadar reflectivity profiles of 154 hail cells have been investigated. An average profile (the hail profile) has been derived. A global method has been used since the hail profile is designed to be applied to global hail parameters. Maximum reflectivities are found at h0 ? 1 km, where h0 is the height of the 0°C isotherm. The change in reflectivity reaches 3 dB km?1 at h0 ? 2 km and for 60 dBZ. This finding agrees with a theoretical profile based on the melting of hailstones. Above h0 the radar reflectivities decrease continuously with a rate of ?1 to ?2 dB km?1.
dc.publisherAmerican Meteorological Society
dc.titleRadar Hall Profiles in Switzerland
dc.typeJournal Paper
dc.journal.volume25
dc.journal.issue7
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1986)025<1002:RHPIS>2.0.CO;2
dc.journal.fristpage1002
dc.journal.lastpage1011
dc.treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 007
dc.contenttypeFulltext


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