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Last modified
7/28/2009 2:32:16 PM
Creation date
4/11/2008 3:38:33 PM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
85-5071
Title
Cooperative Weather Modification Research Program - 1985 Analysis Plan
Date
1/1/1985
State
UT
Weather Modification - Doc Type
Report
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<br />. <br /> <br />Experiment 1: Mesoscale atmospheric kinematics <br /> <br />. <br /> <br />Lead Scientist: Alexis B. <br />Participating Scientists: <br /> <br />Long, DRI <br />Patricia A. Walsh, DRI <br />Robert A. Kropfli, WPL <br />Don A. Griffith, NAWC <br /> <br />. <br /> <br />The objective is to descroibe the airflow on the smaller mesoscale <br /> <br />in the vicinity of the Tushar Mtns to establish the kinematic context on <br /> <br />this scale of cloud formation alnd precipitation development. NCAR C- <br /> <br />. <br /> <br />band radar Doppler radial vell:>city data will be primary. Similar data <br /> <br />from the WPL Ka-band radar m.ay be used to confirm wind estimates near <br /> <br />that radar, and trajectories of constant volume balloons will provide <br /> <br />.. <br /> <br />independent supplementary information on wind velocities. The radar <br /> <br />data will be examined for effE~cts of the Tushar Mtns barrier on the <br /> <br />speed and direction of the airflow at various levels. <br /> <br />Of particular <br /> <br />-- <br /> <br />interest is any channeling of the flow, for example, in a low level jet <br /> <br />around the mountains instead of up and over them. Convection present in <br /> <br />the upper parts of the clouds over the mountains may be observed to have <br /> <br />. <br /> <br />a similar effect. These blocking effects may also be observed in calcu- <br /> <br />lated values of air convergence in the vicinity of the mountains. The <br /> <br />radar data will also be examined for changes of wind speed and direction <br /> <br />. <br /> <br />with height not induced by topography. Such changes may be related to <br /> <br />the advection of warm or cold air into the research area at various <br /> <br />levels due to synoptic scale systems but as modified by local mesoscale <br /> <br />. <br /> <br />disturbances. Wind shifts seen in the radar data may be used to confirm <br /> <br />frontal passages through the research area identified from other data <br /> <br />sources. <br /> <br />. <br /> <br />.\ <br /> <br />23 <br />
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