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<br />- 34" - <br /> <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 />Phase II - Part B, the network will be converted again to snow-rate sensing. <br /> <br />The compre ssed- scale weighing gauge at the laboratory has been in <br />operation throughout the winter and spring; its reduced data are ~hown in <br />Table II. <br /> <br />Climatological station data for the period 1 November 1965 through <br />1 May 1966 are listed in Appendix D, All stations are within the radius of <br />about 40 miles of Steamboat Springs, an.dtheir locations were shown in Fig- <br />ure 5. <br /> <br />METEOROLOGICAL DATA <br /> <br />Wind and tempe rature from the 5 meteorological stations in the net- <br />work have been collected throughout the period from 1 July 1965 through 1 <br />May 1966; Appendix D lists pertinent data for each storm period. Tempera- <br />ture data from the 7 daily climatological stations is also included in Appendix <br />D. <br /> <br />Teletype se:rvices A and C and the U. S. Weather Bureau FAX charts <br />provided synoptic data for analysis throughout the period of interest. <br /> <br />Radar PPI photos were made during each storm, although the radar <br />was used primarily for wind tracking purposes. Operation of the surplus ra- <br />winsonde equipment wa~ not satisfactory, and we were forced to fall back on <br />the use of U. S. Weather Bureau data from Grand Junction, Denver, Lander, <br />and Salt Lake City. <br /> <br />HYDROLOGICAL DAT A <br /> <br />Ridge station snowcourse runs began on 19 November 1965 and contin- <br />ued through 1 May 1966. The ridge thaw began in mid-April and values be- <br />yond these dates have not been used for analysis purposes. <br /> <br /> <br />Stream gauge data are available from the three newly-installed stream <br /> <br />gauge s for all of the spring run-off period. <br />