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<br />we are able to obtain a better feel for the overall meteorological <br />conditions prior to and during operations. Although TV provides <br />local area forecasters' analysis, breaking news about weather <br />warnings and NEXRAD radar displays, TV is not relied upon as much <br />as WKWMP sources of information, that is, our own radar, personal <br />observations, Internet radar displays and DTN. <br /> <br />In order to reduce hail effectively, it is very important to <br />be able to identify a severe storm early in its growth stage and to <br />begin seeding it as quickly as possible. Recognition of non-severe <br />storms as opposed to potentially destructive ones requires a certain <br />degree of expertise. At some point WKWMP pilots 'and meteorologists <br />all acquire an ability to distinguish visually between these two <br />types of clouds with a fairly high level of reliability...a very <br />important aid in getting flights launched early. We prefer not to <br />wait until high radar reflectivity in clouds is seen on radar <br />before launching a seeding plane. In rapidly growing clouds, cloud <br />droplet sizes are not large enough to be "seen" on radar until <br />relatively late after the initial development of a severe storm. <br />WKWMP personnel watch for this rapid, vigorous storm growth in order <br />to . be able to deploy in the shortest time possible. Radar does <br />become an indispensable tool in the identification and tracking of <br />severe storms once they form and at night. <br /> <br />WKGMD *1 owns all the equipment used on the WKWMP. The type of <br />radar systems used by the WKWMP are the Enterprise Electronics <br />Corporation (EEC) WR-100, a 5-cm wavelength model similar to many <br />weather radars in use previously by the National Weather Service, <br />which have been replaced rather recently by the 10-centimeter <br />--waveloengt-h~NE-}fRAD-Doppler- systems. - ---- ___u <br /> <br />U&ing a computer-interfaced radar system allows us to quickly <br />analyze clouds for hail potential. The height of the 45 dBZ <br />intensity' contour within a cloud is - evaluated against a "hail <br />threshold" computed daily. The height of the 45 dBZ intensity level <br />within clouds is used as a test for determining the crop-damaging <br />hail potential in storms and its destructive potential relative to <br />another storm. It provides definitive information which is crucial <br />in making operational decisions regarding aircraft guidance. Output <br />is displayed in colored contours on a monitor. The techniques to <br />determine hail potential in clouds, employed by the WKWMP, have been <br />used continuously since 1985. Although one person can operate the <br />system, it works best if the meteorologist concentrates upon <br />aircraft operations in progress while his assistant operates the <br />computer and collects weather data updates for the meteorologist's <br />examination. During operations the meteorological assistant also <br />moves radar data to the Internet and into a looping display showing <br />a short history of storm movements for the scrutiny of the radar <br />meteorologist. The information acquired by the assistant during <br />operations provides much-needed meteorological input for effective <br />aircraft guidance. <br /> <br />18 <br />