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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 />__i___ <br /> <br />response, Governor Larrm directl:<1 the developnent of a orougnt Response <br />Plan to specify tasks, organizational arrangements and operations of state <br />government under drought conditi.ons (Iarrrn, 1981). <br /> <br />'!he State Weather Modification Advisory Committee (composed 0,( Ll.'JE: <br />scientists and five ranchers and farmers) met in January 1981 to discuSS <br />the possible use of seeding if the drought persisted. The Committee i8~t <br />that Colorado stood the best chance of benefiting from wintel- cloud <br />seeding only if programs were well conceived, conducted on an ongulng <br />basis, and evaluated thoroughly. It did not favor hasty implenentaLioL _L <br />an emergency seeding program because of doubts about the effectiveness Jf <br />seeding during dry periods and the inability to evaluate short-term <br />programs adequately. <br /> <br />The Department of Natural Resources presented this view at a jOl.:1t <br />meeting of the state House and Senate Committees on AgriculturE: and <br />Natural Resources in late January. Thus, although the' drought lasted <br />until March on the plains and later in the mountains, the state did fice <br />fund a seeding program for drought relief in 1981. Ski areas, wate:r <br />users, local governments and businesses, however, did fund progrcillls HI tr..:, <br />southwestern San Juan and central mountain areas. <br /> <br />RESEAOCH APPROACH AND RESULTS <br /> <br />Data Availability and Limitations <br /> <br />Establishing a climatology of seedable storms requires not only <br />criteria for seedability but also a method to identify storms to wnich toe <br />criteria could be applied. Storms can be identified from pLecii?ita\:.~.;;: <br />data but these data are not often recorded in the remote areas or h~gh <br />altitude regions where most of the snow falls (Klazura, 1982). Currently, <br />therefore, the only practicable way to identify storms is from wee. r:~H.:.:. <br />balloon (rawinsonde) soundings.. These soundings provide vel tical ?ro;; ~le:; <br />of temperature, humidity, and 'vlind speed and direction. Alt,ough i-'iE:Y":dn <br /> <br />7 <br />