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<br />. <br /> <br />20 elll 5-1 LIFT <br />TOTAL DYNAMIC POTENTIAL <br />... <br /> <br />/ <br />/ <br /> <br />. <br /> <br />10 cm 5-1 LIFT <br />TOTAL DY~A~IlC POTENTIAL <br /> <br />..P, <br />.,J <br />, <br /> <br />/ <br />/ <br /> <br />. <br /> <br />NO LIFT <br />TOTAL DY~A\lIC POTENTIAL <br />'.'] <br />.. <br /> <br />" <br /> <br />.. <br /> <br />/ <br /> <br />/ <br /> <br />/ <br /> <br />~ WI.' <br /> <br />.. <br /> <br />u <br /> <br />, <br />~ <br />~ <br />z <br />" <br />e <br />~ <br />o <br />~ <br /> <br />/ <br /> <br />/ <br /> <br />.~ <br /> <br />/ <br />;/ <br /> <br />.'j <br /> <br />~ .'j <br />, I <br />~ ....1 <br />z <br />:::: .. <br />e <br />. <br />~ <br />. <br /> <br />"1 <br />~ .,J <br /> <br />o. <br /> <br /> <br />< <br />, <br />.'J <br />, o. <br /> <br />E 1:1.0 <br /> <br />.. <br /> <br />......1 <br /> <br />.., <br /> <br />... <br /> <br /> <br />... ....D 111.. .. WI.' <br />TOlN.l"tlT(IITll'lL lUll ~t <br />~AT VS MOD TOTAL RAINFALL <br /> <br />.. <br /> <br />,., <br /> <br />II.' <br /> <br />.. <br /> <br />.. <br /> <br />., <br /> <br />.c.D ..... .... ,.,.. 00. <br />TOTI\.I'OU"JII\.""''*'J <br />VS \100 TOT..\L RAINFALL <br /> <br />.... <br /> <br />'1"1 <br />/ <br />" <br />u';.. <br /> <br />... <br /> <br />.. <br /> <br />.. <br />!'II. <br />RAINFALL <br /> <br />., <br /> <br />,o..,~ <br /> <br />k:: <br />I.D ,Q,D ;11.0 lEI.. 00.. <br />__TOT' I'{)TO<Tl"- ,....) <br />NAT VS MOD TOTAL <br /> <br />.. <br /> <br />SAT <br /> <br />Q.' <br /> <br />M.' <br /> <br />/ <br /> <br />'] <br /> <br />....'1 <br /> <br />Q <br /> <br />// <br /> <br />-'1 <br /> <br />XIIU1 <br />'la.., <br /> , <br />'...., <br /> I <br /> <br />IoU-f <br /> <br />I <br />. <br /> <br />M.' <br /> <br />-. <br /> <br /> <br />'.. <br /> <br />''''.' <br /> <br />~ <br />. <br />iI <br />. <br />. <br />~ <br />. <br /> <br />1 <br /> <br />. <br /> <br />/ <br /> <br />,\11.. ~ <br /> <br />I <br />..,.~ <br />, <br /> <br />. <br /> <br />~ <br />! <br />" <br />. <br />. <br />f <br />. <br />;; <br /> <br />/ <br />/ <br /> <br />/ <br /> <br />~ <br />. <br />iI <br />. <br />f <br />. <br />~ <br />. <br /> <br />.. <br /> <br />, <br />../1I <br />/ <br />.^ <br />.. <br />. <br /> <br />., <br />~o _~ _. ~ _ IWI ~D ... _.~,~.~. <br />TOTI\.IMI.,.ilU..I....:~T 'OTI\ ""I""'" ,,.., ""f TOT"-iIlI'\l""!U.I....,,,,.1 <br /> <br />figure 2. Effect of IAesosc"'e lifting on total dynlllll1c potential (total cloud depth of all clouds per case) and total rainfall for cases with <br />observed mesoscale triggers at Goodhnd. Kansas in 1976. lifting increases frOlll 0 to 20 CII S.I frOll left to right. Note that both the nUllltler of <br />events and llI4gnltude of effect increase as lifting increases. The 45. line indicates a one-to-one relation between natural and IIOdified (1.e <br />dynallic seeding hypothesis) events. <br /> <br />-, <br /> <br />~, <br /> <br />-. <br /> <br />_. <br /> <br />. <br /> <br />. <br /> <br />~~ <br />m p <br /> <br />. <br />, <br /> <br />.. <br />