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contributor authorZiegler, Conrad L.
date accessioned2017-06-09T14:25:46Z
date available2017-06-09T14:25:46Z
date copyright1985/07/01
date issued1985
identifier issn0022-4928
identifier otherams-19090.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4155168
description abstractThe air flow in convective storms, the force that regulate the flow, and the processes that produce hydrometeors of various kinds are all being studied intensively by meteorologists using Doppler radar observations. The research reported here proceeds from the observed motion through accompanying thermodynamic and micro-physical processes to the analysis of hydrometer content and thermal fields in thunderstorms. A three-dimensional numerical kinematic cloud model employing Doppler wind fields is developed and used to diagnose temperature and mixing ratios within a thunderstorm. The microphysical parameterization includes stochastic coalescence effects in warm clouds as well as well- and variable-density dry hail growth. Known fields from a dynamically simulated cloud are used to establish the accuracy of the retrieval scheme. Real data tests indicate good agreement between retrieved and observed radar reflectivities, qualitative dynamic consistency between observed winds and retrieved buoyancies, and the model's ability to partition liquid and solid hydrometeors. A modification of weighting factors in the variational multiple Doppler analysis changes the vertical motion field and improves the verification of retrieved reflectivities. This analysis sensitivity emphasizes the great influence of the input wind field on retrieved thunderstorm variables.
publisherAmerican Meteorological Society
titleRetrieval of Thermal and Microphysical Variables in Observed Convective Storms. Part 1: Model Development and Preliminary Testing
typeJournal Paper
journal volume42
journal issue14
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1985)042<1487:ROTAMV>2.0.CO;2
journal fristpage1487
journal lastpage1509
treeJournal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 014
contenttypeFulltext


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