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dc.contributor.authorHerman, Benjamin M.
dc.contributor.authorBattan, Louis J.
dc.date.accessioned2017-06-09T14:12:40Z
dc.date.available2017-06-09T14:12:40Z
dc.date.copyright1961/08/01
dc.date.issued1961
dc.identifier.issn0095-9634
dc.identifier.otherams-14750.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150346
dc.description.abstractCalculations of the normalized back-scattering cross-section, σb, of ice spheres surrounded by shells of liquid water have been made from an extension of the Mie theory to a two-layer model. Curves of σb as a function of the thickness of the liquid-water shell are presented for various-sized spheres for 3.21, 4.67 and 10.0 cm radiation. It is shown that, depending upon the size of the sphere and the wavelength of the incident radiation, the back-scattering may either increase or decrease as the ice acquires a liquid-water shell. For certain-sized spheres, interference phenomena, which in some instances may lower the value of σb by several orders of magnitude, are in evidence during the course of melting.Comparisons are made between the theoretical results presented here and experimental measurements of σb for melting ice spheres performed by Atlas et al (1960).
dc.publisherAmerican Meteorological Society
dc.titleCALCULATIONS OF MIE BACK-SCATTERING FROM MELTING ICE SPHERES
dc.typeJournal Paper
dc.journal.volume18
dc.journal.issue4
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1961)018<0468:COMBSF>2.0.CO;2
dc.journal.fristpage468
dc.journal.lastpage478
dc.treeJournal of Meteorology:;1961:;volume( 018 ):;issue: 004
dc.contenttypeFulltext


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