| contributor author | Beard, K. V. | |
| contributor author | Jameson, A. R. | |
| date accessioned | 2017-06-09T14:23:40Z | |
| date available | 2017-06-09T14:23:40Z | |
| date copyright | 1983/02/01 | |
| date issued | 1983 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-18516.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4154530 | |
| description abstract | A theory for canting has been developed from the response of raindrops to shear produced by homogeneous, isotropic turbulence. The model predicts small canting angles, with the tangent of the angle having a Gaussian probability distribution about a mean value of zero. Previous reports of large canting angles above the surface layer were based upon interpretations of microwave measurements which were found to be sensitive to the assumed drop shapes and size distributions. However, past measurements using a circular polarization radar technique, sensitive to canting but not to drop shapes and distributions, yielded a narrow distribution of canting angles with a mean near zero in agreement with theoretical expectations. | |
| publisher | American Meteorological Society | |
| title | Raindrop Canting | |
| type | Journal Paper | |
| journal volume | 40 | |
| journal issue | 2 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1983)040<0448:RC>2.0.CO;2 | |
| journal fristpage | 448 | |
| journal lastpage | 454 | |
| tree | Journal of the Atmospheric Sciences:;1983:;Volume( 040 ):;issue: 002 | |
| contenttype | Fulltext | |
