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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 /> <br />3.1.5 <br /> <br />Summary <br /> <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 />I <br />I <br /> <br />From the descriptions of the weather episodes in Appendix <br />A, it is evident that most of the episodes were related to <br />the passage of synoptic-scale weather systems. Fortunately, <br />these were rather numerous and ran the gamut from heavy precipi- <br />tation producers to none and from those episodes that exhibited <br />a significant amount of SLW to some that had very little. <br />During the field season, the precipitation total was just <br />a little above normal for the period but a greater than normal <br />number of storms did pass through the area. There was a strong <br />tendency for the westerly flow from the Pacific Ocean to be <br />split with several of the storms entering the western states <br />at relatively low latitudes. OVerall, the flow was more meridional <br />than zonal leading to a preponderance of plunging type storm <br />systems. Some of these produced significant precipitation <br />and one was in the 20-year storm class. For these reasons <br />it may be difficult to judge just how representative these <br />episodes are of a typical winter period of comparable length, <br />but climatological data presented in a subsequent section <br />(Section 3.2) suggests that except for the greater number <br />of storm days than usual (noted above) the period was fairly <br />typical for any winter period. <br /> <br />Table 3-1 was prepared as an aid in summarizing the most <br />significant features of the 16 episodes in regard to developing <br />a storm and seeding climatology for the Arizona Mogollon Rim. <br />For each of the episodes the table lists: 1) the Medina weather <br />type, 2) the episode duration (in hours) as determined by <br />the presence of SLW at Happy Jack and/or precipitation recorded <br />in the network gauges, 3) the number of hours that SLW (equal <br />to or greater than .01 mm per hour) was recorded at Happy <br /> <br />3-10 <br />
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