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Last modified
7/28/2009 2:40:29 PM
Creation date
4/24/2008 2:51:22 PM
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Weather Modification
Title
Preparation of Weather Forecasts for Winter Orographic Cloud Seeding Operations in the Colorado Rockies
Date
12/1/1982
State
CO
Weather Modification - Doc Type
Report
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<br />~ <br /> <br />.....'~ <br /> <br />v-j~, <br /> <br />. <br /> <br />,.> <br /> <br />PREPARATION OF WEATHER FORECASTS FOR WINTER OROGRAPHIC <br />CLOUD SEEDING OPERATIONS IN THE COLORADO ROCKIES <br /> <br />by <br />WESTERN WEATHER CONSULTANTS, INC. <br /> <br />December 1982 <br /> <br />The most favorable meteorological conditions for the augmentation of pre- <br />cipitation from cold orographic cloud systems by seeding with ground-based <br />silver iodide (AgI) generators can be separated into four general physical <br />categories, namely; water available, nuclei available, mixing available and <br />time available. The meteorological conditions under the four categories can <br />be determined from rawinsonde data and all other available National Weather <br />Service (NWS) data. The following describes how WESTERN WEATHER CONSULTANTS, <br />INC. (WWCI) evaluates each of these basic categories to arrive at a forecast <br />for cloud seeding operations. <br /> <br />1. WATER AVAILABLE <br /> <br />The amount of liquid water available in a cloud is key to determining! seed- <br />ability; the greater the cloud water content, the more water that can poten- <br />tially precipitate out of a cloud system. Parameters useful in estimating! the <br />available water are cloud base height, cloud depth and cloud base moisture. <br />WWCI has established the following guidelines in evaluating this category: <br />Cloud Base Height must be lower than 1,000 ft. above the <br />average elevation of the mountain crest. <br />Cloud Depth must be in excess of 2,000 ft. <br />Cloud Base Moisture must be in excess of 1.5 gm/kgm. <br />The most recent rawinsonde from Grand Junction (GJT) and cloud observations <br />from NWS reporting stations near the target areas are examined to determine the <br />current cloud base height and depth. The base of the lower cloud layer is <br />usually easily identified; on the GJT rawinsonde, the base is determined as the <br />point where the temperature-dew point spread is less than 30C. To estimate <br />cloud depth, we use the rule of thumb that the relative humidity must be 85 <br />percent or greater to be identified as a cloud region. The cloud base moisture <br /> <br />~ <br />
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