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Last modified
7/28/2009 2:36:54 PM
Creation date
4/16/2008 10:28:34 AM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
0-07-81-V0144
Project Name
South West Drought Project
Title
Operational Weather Modification - Volume I: A Seminar Series
Date
9/1/1981
State
OK
Weather Modification - Doc Type
Report
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<br />-18- <br /> <br />~ <br /> <br />1. Introduction <br /> <br />i <br /> <br />The dry years of the middle 1970's have stimulated weather <br />modification activities (cloud seeding for the purpose of in- <br />creasing rainfall from convective clouds) over parts of the <br />Middle West and High Plains agricultural areas. These same <br />areas are often frequented by severe weather (excessive rains, <br />large hail, damaging winds and tornadoes) during most of the <br />crop growing season. When there is sufficient advance know- <br />ledge of the threat of severe weather, the field managers may <br />shut down cloud-seeding operations to ensure the safety of <br />project personnel and to avoid the charge that the seeding <br />caused or enhanced the severe weather. This possibility was <br />raised with regard to the flood-producing storm at Rapid City <br />in 1972 (St. Arnand et a1., 1972: Dennis et al., 1973). <br />Because of limitations in the data used for this study, <br />several basic assumptions had to be made in the development <br />of the suspension criteria. All June rainfall was assumed to <br />be convective. The seeding opportunity day was assumed to be <br />a day with seeding opportunities, i.e., a day with rainfall <br />anywhere within an operational area. Therefore, cloud seed- <br />ing is assumed to be much more effective in the augmentation <br />of natural rainfall than in the initiation of rainfall on <br />days in which natural rainfall would not have occurred. <br />Support for these assumptions is found in the 1arge- <br />amplitude June diurnal rainfall frequency and amount curves <br />for the Dodge City area (Fig. 2). Most rain fell during the <br />late afternoon and early nighttime hours. This period is <br />generally considered as the period most favorable for convec- <br />tive rainfall. Further, the frequency curve shows that fewer <br />than 20 storms occurred during the late morning (0900-1200 LST), <br />thus establishing that multiday storms were relatively uncommon. <br />Thus, given that rain occurred during a 24 h period (0700-0700), <br />the rainfall most likely occurred during the convective period <br />which is most favorable for seeding opportunities. <br /> <br />~ <br />
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