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WMOD00284
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Last modified
7/28/2009 2:32:39 PM
Creation date
1/8/2008 12:16:50 PM
Metadata
Fields
Template:
Weather Modification
Applicant
Thompson, J.R., G.W. Wilderson, and D.A. Griffith, North American Weather Consultants
Sponsor Name
USBR
Title
Cloud Seeding Data Collection, and Analysis Assoc. with the Colo River Augmentation Demonstration Program
Prepared For
USBR, Divison of Atmospheric Research
Prepared By
Thompson, Wilderson, Griffith
Date
12/1/1987
State
AZ
Weather Modification - Doc Type
Scientific Study
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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />are likely to be composed of either stable orographic clouds <br />(generally the best candidates for seeding provided the air <br />mass temperature is not too cold) or at other times may contain <br />embedded wet convective clouds. <br /> <br />3.1.2 <br /> <br />Episode Definition <br /> <br />with this background, the weather patterns which affected <br />the Arizona Mogollon Rim region during the mid-January to <br />mid-March 1987 field season were examined to allow a comparison <br />with the earlier climatological analysis. One of the goals <br />was to attempt to determine whether there were significant <br />differences in the production of supercooled liquid water <br />(SLW) from one weather type to another. If there was, this <br />might be quite useful in making decisions about the seedability <br />of a given storm. Also, it was hoped that the analysis might <br />provide additional insight into whether certain phases of <br />the weather type were more seedable than others, e.g., a period <br />(or periods) when more SLW was being produced. <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />storm episodes were defined as generally continuous periods <br />of SLW and/or precipitation, and having no interval longer <br />than 2 hours during which neither some precipitation or SLW <br />was recorded. Integrated SLW measurements (in mm per hour) <br />were made by the Bureau's dual-channel microwave radiometer <br />near the Happy Jack Ranger Station. This instrument was operated <br />in a vertically pointing mode with.readings of liquid water <br />and water vapor made at two minute intervals. These readings <br />were then averaged for each hour for each of the episodes. <br />Average hourly values less than .01 mm were considered to <br />be in the noise range of the instrument and were not used <br />in determining the episode SLW average. However, since they <br /> <br />3-6 <br />
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