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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 />CSU Intemet site (htt)1:/lrams,almos,cok'slaIC.OOll/rcahin.1ci). Two-hourly pro,llIcls will <br />also he availahle for slIch varial1lcs WI winds rOT transport and diffusion calculations, <br />temperature. relative humidity. and mixing ratios for each hydrometer species. <br /> <br />o <br /> <br /> <br />- <br /> <br />y(kl,..) <br /> <br />00 <br /> <br />.50 <br /> <br />-100.- <br /> <br />~ 1:';100 <br /> <br />-150 <br /> <br />-100 <br /> <br />.... <br /> <br />o. <br /> <br />. (~m) <br /> <br />F1Illlr".J. Propo'\.Cd domain for RAMS tine grid (J-km gri,l spacing). Topography is <br />shaded at 200-m intervals. Towns (l.re-Her mI. S~llcl sites (X). Sl1nwcnUI1iC sites (+1. <br />co-IOCn1cd Snolcllsrwwcoursc sites I.) and 2002-200J winleT season ice nuclei gc[\cratnr <br />sites (A) arc shown. Thcsc~'<linl!largctarcaisfromFig\lrc2. <br /> <br />011 dayswhcllclouds arc present, we proposcto pcrlonnpO:;I.ful'l'<;;I'I-.Ulalysishy <br />rcpcatinglhc forccaslshyaddingoourccsoflFN conccnlratillns hnSC\1 0 nloeationsand <br />ice nuclei genernlof outl'futs provided to us hy Larry IIjermstad. This analysis will <br />inchule not only the DWD scctlingollCf:llions, but also that uverlhe Vail Ski Area <br />sc~.ding prograllllhal is upwind of the DW[) !In.gram area. Agl will he a,hk,l as II <br />scp:lratcpredictedsl'ociesinRAMS,IIHlhaveitsunlqucaclivalj"nchar:lCtcnslicsas <br /> <br />11.12 <br />