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Last modified
7/28/2009 2:40:48 PM
Creation date
4/24/2008 2:55:34 PM
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Template:
Weather Modification
Project Name
Project Skywater, Sierra Cooperative Pilot Project
Title
Project Skywater, Sierra Cooperative Pilot Project - Fall 1984 Status Report
Date
12/1/1984
Weather Modification - Doc Type
Report
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<br />2 <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 />I <br />I <br />I <br />I <br />I <br /> <br />studies should be part of the program and the general public should be <br />kept informed of SCPP activities. <br /> <br />On the basis of' a contract design study awarded in 1975 and completed <br /> <br />in 1976 by MBAssociates, the ARB (American River Basin) was selected <br /> <br />as the primary study area. Figure 1 outlines the location of the ARB <br /> <br />and details some of the important characteristics of the basin as relates <br /> <br />to size, precipitation and runoff. <br /> <br />As most of California, including the ARB, has a Mediterranean climate, <br />almost all (97%) of the annual precipi ta tion in the ARB falls between <br />October and May with 78% of the annual precipitation falling in the colder <br />winter months of November thru March. The storms affecting this region <br />usually move in off the Pacific having had long residence times over <br />the ocean. Freezing levels usually range from 900 m (3000 ft) to 3000 m <br />(10,000 ft) above sea level. Warmer storms usually originate in the <br />Southern Pacific. Colder storms, with freezing levels as low as 300 m <br />(1000 ft) come from the Gulf of Alaska. These storms often stagnate <br />just off the coast bringing showery unsettled weather for several days. <br /> <br />The average annual precipi ta tion totals from the valley floor to the <br /> <br />Sierra crest and beyond Lake Tahoe are shown in Figure 2. Note that <br /> <br />the precipitation on the west (upwind) side increases with elevation, <br /> <br />but with little change from Blue Canyon to the crest. It then decreases <br /> <br /> <br />rapidly downwind of the crest due to evaporation of cloud particles in <br /> <br /> <br />the subsiding, and hence, warming air. <br />
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