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<br />. <br /> <br />I <br /> <br />I <br /> <br />from the release of latent heat (primarily from freezing). and from redistribution of <br />condensed water \\'ithin the targeted cloud tUITets. <br /> <br />~ <br /> <br />_11..... <br />...-.; <br /> <br /> <br />1)0...4--",.,.'_ <br />~ <br /> <br />- <br /> <br />.-- <br />.---) <br />IS'C-___________ <br />I <br />-'- <br />..~ . I <br />'- <br />j <br />O"C---- ------ <br /> <br />"" <br />.."-"I..,T...,..,.,.... <br />......- <br />o,-*""'~ <br />.-- <br />o~..t:.,-___ <br /> <br /> <br />/t: <br />pj <br /> <br />j <br /> <br />,.v <br /> <br />. <br />. <br />. <br />. <br /> <br />"....,__10.,..'- <br />...- <br /> <br />FiKlIrf! I. lIail.\'Ul'pre.uion CO!1('epls.from WJfO Technical Document No. 76-1. [1)1)6. <br /> <br />3.1.2 E\'idclu:e of cloud s('('dill~ errCl'Cs <br /> <br />Progress in the numerical simulation ofhailstonns and hailstone evolution has <br />occurred. and is disclIssed below in Section 3.4. Contrary to statements in the NRC <br />rcpon.lhcre arc reasonable models that simulate the dcn:lopmcnt of hail in realistic <br />hailstorm environments. Cloud seeding simulations show the crfects of carly rainout and <br />bcnclicial competition in reducing hail from relatively ellicient hailstorms. but the <br />possible increase of hail and rain from some relatively inellicienl storms. The models <br />also show the lot'ation of hail embryos close to the forward region of the major updraft. <br />The major grO\\lh of the icc particlcs occurs in high liquid \vatc.:r regions between _SoC <br />and -3SoC. usually between _lOoe and -250C. Trajectory analyses indicate that particlcs <br />that grow to relati\'c1y large size begin their major gro\\ th cycle in a \'ery narrow ribbon- <br />like region in an area ofwcak upJral1 near the updralVdowndraft interface on the forward <br /> <br />I" <br />