contributor author | Jameson, A. R. | |
contributor author | Heymsfield, A. J. | |
date accessioned | 2017-06-09T14:21:41Z | |
date available | 2017-06-09T14:21:41Z | |
date copyright | 1980/08/01 | |
date issued | 1980 | |
identifier issn | 0022-4928 | |
identifier other | ams-17974.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4153927 | |
description abstract | Extensive comparisons of dual-wavelength (10 and 3 cm) radar data with observations at the ground and penetration aircraft (T-28) measurements of hail in a Colorado storm show that positive hail signals (10 cm reflectivity factor exceeds that at 3 cm) are well correlated with the presence of hail ? 1 cm diameter. Widespread areas of negative hail signals (3 cm reflectivity factor exceeds that at 10 cm) found above the melting level are correlated with the presence of subcentimeter graupel. It is possible, therefore, to discriminate two sizes of particles based on dual-wavelength radar measurements. This finding is exploited in Part II of this work to investigate the evolution of graupel into hail. | |
publisher | American Meteorological Society | |
title | Hail Growth Mechanisms in a Colorado Storm. Part I: Dual-Wavelength Radar Observations | |
type | Journal Paper | |
journal volume | 37 | |
journal issue | 8 | |
journal title | Journal of the Atmospheric Sciences | |
identifier doi | 10.1175/1520-0469(1980)037<1763:HGMIAC>2.0.CO;2 | |
journal fristpage | 1763 | |
journal lastpage | 1778 | |
tree | Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 008 | |
contenttype | Fulltext | |