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Last modified
7/28/2009 2:37:18 PM
Creation date
4/16/2008 10:30:31 AM
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Template:
Weather Modification
Title
Potential Opportunities for Precipitation Augmentation in the Eastern Tennessee Valley
Date
2/1/1988
Weather Modification - Doc Type
Report
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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 />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />4. Specify the design of Phase II. This section outlines the objectives <br />and cost of a one-time intensive 3-month field program to obtain <br />detailed physical measurements on variDus aspects of the clouds in the <br />eastern TVA region. The purpose of this effort would .be to confirm with <br />in situ observations the seeding potential in candidate clouds specified <br />in Phase I, and to develop seeding hypotheses for a Phase III demonstra- <br />tion program. <br /> <br />2.0 Report Summary and Recommendations <br /> <br />A review has been made of the available meteorological data relevant in deter- <br />mining the potential for precipitation augmentation over the eastern TVA region <br />during the 3 spring months, March, April and May. Six years of data were used <br />in the study, 1982-1987. The data show that cloud systems inducing precipita- <br />tion transition from large synoptically included stratiform cloud systems to <br />individual convective cloud or convective cloud systems during this 3-month <br />period. <br /> <br />It has been found that the relatively shallow cold orographic cloud present over <br />the eastern TVA region for about 70 to 80 hours each March and April offers a <br />very real potential for precipitation increases through application glaciogenic <br />seeding material released from ground generators or by aircraft. Given that a <br />little over 70 percent of the precipitation which falls during March and April <br />subsequently runs-off, there is adequate justification for further exploration <br />of these cloud types to improve seedability estimates and seeding strategies. <br /> <br />Convective clouds that develop on approximately half the days in May, generally <br />induced ~y diurnal heating over the southern Appalachians, may also offer poten- <br />tial for precipitation increases. The available data show these convective <br />clouds are relatively warm-based (CST +100C). Past cloud seeding'programs and <br />application of 1-D cloud model suggest these clouds could be induced to increase <br />their vertical height by application of dynamic seeding principles. However, <br />model results would imply only the relatively small, moderate growth convective <br />clouds would respond positi'vely. These would imply that clouds have to be <br />selectively treated and the effects would be limited to a small portion of the <br />total target area. This conclusion and the fact that only 50 percent of the May <br />rainfall runs off show that further evaluation is necessary before final conclu- <br />sions can be reached on the advisability of seeding these clouds for precipita- <br />tion increases. <br /> <br />The cost effectiveness of cloud seeding was estimated using preliminary projec- <br />tions of basin runoff based on anticipated precipitation increases and projected <br />costs of an op~rational program. The calculations indicate benefit-cost ratios <br />in the range of 3.6:1 to 6.5:1 on an average annual basis. It must be empha- <br />sized that theSe benefit-cost calculations are preliminary until further <br />assessment of cloud seedability and treatment capability is determined. <br /> <br />xv <br />
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