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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 /> <br />" <br />rimIIlJJ m "Y: . ..' ,~ <br />/;!Ifl!l '1IC.~~'X()!1& <br /> <br /> <br />"-- <br /> <br /> <br />L-", <br />2980 <br /> <br />--- <br /> <br />3 ~ <br /> <br />~.. <br />30'10" /'. <br />\ '~'. " <br /> <br />\ <br /> <br />\ <br />\ <br /> <br />, , <br /> <br />~ <br /> <br />.~ <br /> <br />, <br /> <br />J:f(RS <br /> <br />/ <br /> <br />III <br /> <br />~ <br /> <br />,. <br /> <br />\\,.- <br /> <br />"" <br /> <br />.... I-f'-- <br />-~...--. <br />, ., <br />"1; 't. <br />'t. '-" <br />....- - - .-. <br /> <br />Figure 3-1. Same as Fig. -I, except fhr (}fJ()() GMT on 28 February (/7{}() MS/' 27 Feh) /99-1. <br /> <br />IV. 1994 :-OAA.lITAII CASE STlIIIIES <br /> <br />Several experiments from the 1994 NOAA.Ulah field program were identified for intensive <br />analysis by the various researchers The DRI scientists imtially concentrated on cases involving the <br />mobile radiomt.:tcr. The first slom of the field program provided the only mobile radiometer data <br />collected during transects through seeding plumes. Also unique for this case was the collection of <br />radiometer data in tandem with the Utah instrumented van. A second case on 7 February provided <br />the best comparative data between the RRS stationary radiometer and the mobIle radiometer as it <br />made passes across the Wasatch Plateau, and collected some data in a stationary mode on the <br />dowm...ind side of the plateau The third case studIed by DRI, to date, was selected because of <br /> <br />45 <br />