contributor author | Lolli, S. | |
contributor author | Di Girolamo, P. | |
contributor author | Demoz, B. | |
contributor author | Li, X. | |
contributor author | Welton, E. J. | |
date accessioned | 2017-06-09T17:26:28Z | |
date available | 2017-06-09T17:26:28Z | |
date copyright | 2017/04/01 | |
date issued | 2017 | |
identifier issn | 0739-0572 | |
identifier other | ams-85320.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4228754 | |
description abstract | ain evaporation, while significantly contributing to moisture and heat cloud budgets, is a still poorly understood process with few measurements presently available. Multiwavelength lidars, widely employed in aerosols and clouds studies, can also provide useful information on the microphysical characteristics of light precipitation, for example, drizzle and virga. In this paper, lidar measurements of the median volume raindrop diameter and rain evaporation rate profiles are compared with a model analytical solution. The intercomparison reveals good agreement between the model and observations, with a correlation between the profiles up to 65% and a root-mean-square error up to 22% with a 5% bias. Larger discrepancies are due to radiosonde soundings different air masses and model assumptions no more valid along the profile as nonsteady atmosphere and/or appearance of collision?coalescence processes. Nevertheless, this study shares valuable information to better characterize the rain evaporation processes. | |
publisher | American Meteorological Society | |
title | Rain Evaporation Rate Estimates from Dual-Wavelength Lidar Measurements and Intercomparison against a Model Analytical Solution | |
type | Journal Paper | |
journal volume | 34 | |
journal issue | 4 | |
journal title | Journal of Atmospheric and Oceanic Technology | |
identifier doi | 10.1175/JTECH-D-16-0146.1 | |
journal fristpage | 829 | |
journal lastpage | 839 | |
tree | Journal of Atmospheric and Oceanic Technology:;2017:;volume( 034 ):;issue: 004 | |
contenttype | Fulltext | |