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Last modified
7/28/2009 2:39:14 PM
Creation date
4/18/2008 10:01:47 AM
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Template:
Weather Modification
Title
HIPLEX - 1978-79 Operations Plan - Big Spring-Snyder, Texas
Date
4/1/1978
Weather Modification - Doc Type
Report
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<br />.. <br /> <br />4. SEEDING HYPOTHESES FOR TEXAS HIPLEX <br />4.1 CUmulus-Type Clouds <br />Two seeding hypotheses have been developed for the Texas HIPLEX <br />area and are similar to those developed for the Miles City area at the <br />Dillon-Frisco, Colorado, meeting in December. Both of these hyp01~eses <br />will be applied to cumulus mediocris, cumulus congestus, or towering <br />cumulus before echo development while the cloud is growing through the <br />-40C to -lOoC region. The first hypothesis refers to light seeding <br />while the second refers to heavy seeding. These hypotheses are as <br />follows: <br />Hypothesis 1: An increase in the ice crystal concentration <br />through silver iodide seeding in the region where cloud water is present <br />and the temperature is -40C to -lOoC will lead to additional precipita- <br />tion through the base of the cloud. The sequence of processes leading <br />to this increase is hypothesized to be: <br />a. Production of 1-10 per liter ice crystal concentrati.on <br />in the super-cooled water cloud between -40C and -lOoC. <br />b. Freezing of water drops or diffusional growth of the <br />ice crystals to a size where riming can occur. <br />c. Change in cloud liquid water content. <br />d. Accretional growth to precipitation sizes. <br />e. Earlier precipitation development and earlier first <br />echo. <br />f. Fall of precipitation through cloud base. <br />Hypothesis 2: Same statement. as for Hypothesis 1. The sequence <br />of processes leading to this increase is hypothesized to be: <br />a. Production of greater than or equal to 100 per liter <br />ice crystal concentrat.ion in the super-cooled water cloud <br />from -40C to -lOoC. <br />b. Substantial glaciation of the cloud with an associated <br />release of latent heat and buoyancy increase. <br />c. Increases in cloud top heights and subcloud convergence. <br />d. Increased mesoscale moisture flux into the cloud and <br />condensation within the cloud. <br /> <br />.. <br /> <br />e. <br /> <br />Conversion of extra condensate to precipitation. <br />Fall of precipitation through cloud base. <br /> <br />f. <br /> <br />11 <br />
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