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dc.contributor.authorGerhardt, J. R.
dc.contributor.authorTolbert, C. W.
dc.contributor.authorBrunstein, S. A.
dc.date.accessioned2017-06-09T14:12:44Z
dc.date.available2017-06-09T14:12:44Z
dc.date.copyright1961/10/01
dc.date.issued1961
dc.identifier.issn0095-9634
dc.identifier.otherams-14777.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150375
dc.description.abstractBy using laboratory techniques described in a previous paper, results of the measurements of the back-scattering cross-sections of falling water drops and suspended ice spheres are presented for wavelengths of 1.50 and 5.72 cm. As in the earlier study at 3.20 cm, the water-value agreement with the complete diffraction theory of Mie is excellent. Rayleigh values are a good approximation at 5.72 cm out to drop diameters of about 0.35 cm but can be used at 1.50 cm only for drops less than about 0.15 cm in diameter. In addition, recent theoretical evaluations by Herman and Battan of the Mie back-scattering from melting ice spheres are compared with earlier observations made at 3.20 cm. When a constant water film thickness of 0.01 cm is used, the observed back-scattering cross-sections versus drop diameter are in remarkable agreement with theory.
dc.publisherAmerican Meteorological Society
dc.titleFURTHER STUDIES OF THE BACK-SCATTERING CROSS-SECTIONS OF WATER DROPS AND WET AND DRY ICE SPHERES
dc.typeJournal Paper
dc.journal.volume18
dc.journal.issue5
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1961)018<0688:FSOTBS>2.0.CO;2
dc.journal.fristpage688
dc.journal.lastpage691
dc.treeJournal of Meteorology:;1961:;volume( 018 ):;issue: 005
dc.contenttypeFulltext


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