RADAR CROSS-SECTIONS FOR WATER AND ICE SPHERESSource: Journal of Meteorology:;1961:;volume( 018 ):;issue: 003::page 348Author:Stephens, J. J.
DOI: 10.1175/1520-0469(1961)018<0348:RCSFWA>2.0.CO;2Publisher: American Meteorological Society
Abstract: Radar cross-sections for water and ice spheres, evaluated by using the complete Mie theory and the method of Aden, are presented for wavelengths ranging from 0.43 to 16.23 cm. The validity of the Rayleigh approximation is shown as a function of drop diameter, and the temperature dependence is shown for a wavelength of 3.2 cm. Oscillations of the normalized cross-section for water are explained in terms of multipole resonance effects.
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| contributor author | Stephens, J. J. | |
| date accessioned | 2017-06-09T14:12:37Z | |
| date available | 2017-06-09T14:12:37Z | |
| date copyright | 1961/06/01 | |
| date issued | 1961 | |
| identifier issn | 0095-9634 | |
| identifier other | ams-14727.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4150320 | |
| description abstract | Radar cross-sections for water and ice spheres, evaluated by using the complete Mie theory and the method of Aden, are presented for wavelengths ranging from 0.43 to 16.23 cm. The validity of the Rayleigh approximation is shown as a function of drop diameter, and the temperature dependence is shown for a wavelength of 3.2 cm. Oscillations of the normalized cross-section for water are explained in terms of multipole resonance effects. | |
| publisher | American Meteorological Society | |
| title | RADAR CROSS-SECTIONS FOR WATER AND ICE SPHERES | |
| type | Journal Paper | |
| journal volume | 18 | |
| journal issue | 3 | |
| journal title | Journal of Meteorology | |
| identifier doi | 10.1175/1520-0469(1961)018<0348:RCSFWA>2.0.CO;2 | |
| journal fristpage | 348 | |
| journal lastpage | 359 | |
| tree | Journal of Meteorology:;1961:;volume( 018 ):;issue: 003 | |
| contenttype | Fulltext |