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Last modified
7/28/2009 2:40:31 PM
Creation date
4/24/2008 2:52:08 PM
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Weather Modification
Title
Projected Impacts of a Very Large Windpower Complex
Date
9/26/1978
Weather Modification - Doc Type
Report
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<br />economic systems of which it is an important part, Analysis of environmental <br />impact on these higher levels must be considered also, <br /> <br />1. Environmental Impacts of Windfarms <br /> <br />The Energy Research and Development Administration (now emerged into <br />the Department of Energy) examined the impacts of wind machines as one element <br />of the Federal Wind Energy Program. A contract was let with the University of <br />Michigan to study interference in radio, TV, and other communications systems. <br />Battelle Memorial Institute was given a contract to study microclimatic <br />effects and impacts on migratory birds, Preliminary reports of the findings <br />have been published 13, 14 and further reports are due shortly. Howell 15 <br />has examined the environmental impacts of large arrays of individual wind <br />machines aggregated into windfarms, <br /> <br />a. Microclimatic, - The large windfarms projected in this thought- <br />experiment would increase the roughness of the earth's surface in their <br />immediate area, thus affecting both the distribution of wind in the vertical <br />and the details of wind swirl patterns at the ground. These changes would in <br />turn affect the local details in the patterns of tempera ture, prE~cipitation, <br />snow drifting, and evaporation. <br /> <br />The effects of increased terrain roughness have been studied in <br />connection with the microclimatic effect of cities, which roughen the earth's <br />surface to an even greater extent and over eVlen larger areas than would be the <br />case with windfarms. In light to moderate wind, the effects of surfacle rough- <br />ness are relatively trivial. When the wind is strong, one of these windfarms <br />would tend to increase the rate at which air 1within a few tens of meters of <br />the ground mixes with air at higher levels up to a height of as Dluch as 1.5 <br />km, depending upon the strength of the wind and the distribution of temperature <br />aloft. The roughness also decreases the average speed within the turbulent <br />layer. '. <br /> <br />The windfarms would cause some decrease in average windspe4ed and <br />some increase in turbulence above a few tens of meters with relatively little <br />effect closer to the ground where the air is turbulent anyway whenever the <br />wind is strong, <br /> <br />Increased turbulence through a considerable depth above the ground <br />tends also toward a somewhat more even distribution of potential temperature <br />during episodes of strong wind. The range of temperature variation would <br />therefore be somewhat -decreased at such times.. Since the moisture content of <br />the air near the ground normally decreases up..~ard, the mixing would tend to <br />decrease the relative humidity slightly next to the ground and perhaps <br />increase it slightly at the top of the mixing layer several hundred meters <br />higher. <br /> <br />Precipitation from large storm systems, either winter storms or <br />large organized systems of convective clouds in summertime, would be almost <br />entirely unaffected by local changes in surface roughness associated with <br />windfarms. During the weather conditions that: make for small, scatterE!d <br />summertime showers, it is conceivable that the braking effect of the windfarm <br />on the airstream crossing over it could lead to slight local convergenc:e along <br />
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