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<br />28 <br /> <br />PARK RANGE ATMOSPHERIC WATER RESOURCES PROGRAM <br /> <br />STATION DECEMBER 1964 JANUARY 1965 FEBRUARY MARCH APRIL <br />LAB 1 I I I I I I I I II I II I <br />LAB 2 I I I I II I II I <br />MT, HARRIS II I I II I II <br />MILNER I I II I I II I II <br />STEAMBOAT I I II I I II I II <br />CLARK I II I II I II I <br />MAD CREEK I I II I II I II <br />E-MERALD MT, I I III II <br />LUFKIN I II I I II I I I <br />OAK CREEK I II I II I II <br />DRY LAKE II I I I I III II I <br />BUFFALO II I I I III II II <br />FISH CREEK III .11 I I . I /II /I I J <br />LONG LAKE II I I I I III II II <br />BASE CAMP II I I I I I I I II II I II II <br />RABBIT EARS I I I I II I <br /> <br />Figure 40.-Storms Tracked by Precipitation-rate Sensors, December 1964 through April 1965. <br /> <br />also processed at our laboratory for ZnS to deter- <br />mine the natural background concentration of the <br />tracer. A high silver background was found at <br />severallocations-Mt. Lassen, Calif.; Flagstaff, Ariz.; <br />Mammoth Ski Area, Calif.; and Park Range, Colo" <br />where artificial nucleation operations are being con- <br />ducted; no significant ZnS concentrations were <br />found in the samples except for those taken at <br />Steamboat Springs. <br />Natural nuclei data from the Valley View Lodge <br />location were taken throughout the winter and <br />spring twice a day. <br /> <br />Precipitation Data <br />For comparative evaluation purposes, a set of <br />precipitation sensors was installed at the laboratory <br />between 1 December and 15 December 1964. They <br />included an optical sensor, heated tipping-bucket <br />sensor, snow-pillow, compressed scale weighing gage <br />and shielded snow-board. The decision to use the <br />optical sensor for precipitation-rate measurements <br />was made in the first week of January and five units <br />were installed by 15 January 1965. All 15 network <br />stations were in operation by 1 February 1965. To <br />1 May 1965, 26 storm sequences were tracked <br />through the network. Not all stations tracked all <br />storms; figure 40 lists each station and depicts the <br />storms that the station tracked successfully. <br />The network was converted to rain-rate sensing <br />on 1 June 1965; this will be the primary data source <br /> <br />through 1 October 1965 when-in Phase II-the net- <br />work is again converted to snow-rate sensing. <br />The compressed-scale weighing gage at the labora- <br />tory has been in operation throughout the winter <br />and spring. Its reduced data is shown in table 2. <br />Climatological station data for the period 1 <br />November 1964 to 1 May 1965 are listed in Appen- <br />dix D, Section I. All stations are within a radius <br />of about 40 miles of Steamboat Springs, and their <br />locations are shown in figure 5. <br />Other precipitation data were taken for sensor <br />evaluation or spot-check purposes; they are not in- <br />cluded in this report. <br /> <br />Meteorological Data <br /> <br />Wind and teniperature data from the five meteor- <br />ological stations in the network have been collected <br />since mid-January 1965. Dual data are available <br />from the Emerald Mountain site for diffusion pre- <br />diction. Appendix D, Section II, lists pertinent data <br />for each storm period. Temperature data from the <br />seven daily climatological stations is also included <br />in Appendix D, Section I. <br />Teletype Services A and C and the U.S. Weather <br />Bureau FAX charts provided synoptic data for <br />analysis. Complete data are available from 1 <br />January 1965 for the western United States. <br />No useful radar data were obtained during Phase <br />I, except for ground-clutter pictures. The radar is <br />free of clutter for all azimuth angles at 70 mil <br />(_40) elevation. Installation of the radar jrawin- <br />sonde equipment occurred late, for a variety of <br />