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<br />-14- <br /> <br />-15- <br /> <br />typical thunderstorm in and around the Gore Creek Valley is limited <br />to approximately ten squaremiles.1 Using this data, the 10 and 100 <br /> <br />Snowfall Prec1pitation and Snowpack <br />The Soil Conservation Service has kept snowpack and water content <br />records on Shrine Pass since 1942 and on Vail Pass since 1952. Table <br /> <br />year thunderstorm rainfall values ~re: <br /> <br />15 min. <br />30 min. <br />45 min. <br />60 min. <br />24 hrs. <br /> <br />10 YEAR <br />THUNDERSTORM <br />(cum. ins.) <br />.42 <br />.62 <br />.76 <br />.87 <br />1.07 <br /> <br />10DYEAR <br />THUNDERSTORM <br />(cum. ins.) <br />.71 <br />1.07 <br />1.32 <br />1.50 <br />1.85 <br /> <br />II!.1 shows the April 1 and May 1 values recorded at these 10cat1ons . <br />The Shrine Pass station, at 10,500 feet, has an average May 1 snowpack <br />of 55 incheswith19.5 inches of water content. TheaverageApri11 <br />snowpack at the Vail Pass station is 55 inches of snow with 17.9 <br /> <br />TIME FRO~ <br />BEG. OF STORM <br /> <br />The infrequent general rainstorm, which occurs primarily in <br />September and lasts several ho~rs to over 48 hours in some ~ases, <br />has also been developed from Dillon rainfall records. This general <br /> <br />inches of water. The records indicate a maximum snowpack depth occurs <br />at the Vail Pass station somewhat earlier in the year than at the <br />Shrine Pass station. The reasons for this are many and include <br />elevation, siting and aspect. <br />The Soil Conservation Service has made a statistical analysis <br />us1ng data through 1971.18 The resultant 100 year probable return <br />per10d snowpacks and water contents are as follows: <br /> <br />storm may cover a 1.000 square ml1e or larger area. The one-percent <br />probability, 24~hour rainfall from a general storm is 1.89 inches <br />and the corresponding 48-hour value is 2.17 inches. Oncea9ain,the <br />cool autumn temperatures will cause much of this precipitat-on to fall <br /> <br />Station Snowpdck <br />(in.1 <br />Shrine Pass 77 <br />Vail Pass 90 <br /> <br />Water Content <br />(in.) <br />29.0 <br />36.2 <br /> <br />dS snow or hai1 atthehighere1evations. Theadopteddistl'ibution <br />of the general type storm is as follows: <br /> <br />HOURS FROM 10 YEAR GENERAL <br />BEG. OF STORM STORM PRECIPITATION <br />(cum. ins.) <br /> <br />100 YEAR GENERAL <br />STORM PRECIPITAT:ON <br />(cum. ins.) <br /> <br />1 .21 <br />2 .28 <br />3 .33 <br />4 .37 <br />5 .40 <br />6 .44 <br />8 .51 <br />10 .59 <br />12 .67 <br />24 .9l <br />48 1.05 <br /> <br />.44 <br />.58 <br />.68 <br />.76 <br />.83 <br />.90 <br />1.06 <br />1.22 <br />1.38 <br />1.89 <br />2.17 <br /> <br />A revised analysis using data through 1975 would show moderate <br />differences because of the longer recording period. <br />In June 1952, the highest stream discharges on record were at the <br /> <br />Upper Gore, Lower Gore and 81ack Gore Creek stations; the snowpack ~t <br /> <br />Shrine Pass was 22.0 inches on May 1 and 23.7 inches at Vail Pass. <br /> <br />Maximum recorded snowpacks at Shrine Pass and Va11 Pass are 26.7 inches <br /> <br />on April 1. 1965and27.9inchesonMayl,1970,respective1y. <br />