Laserfiche WebLink
<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 /> <br />SUMMARY OF WEATHER AND OPERATIONAL SEEDING OPPORTUNITIES FOR THE 2002-2003 <br />SEASON OF THE V AlL AND BEAVER CREEK SKI AREA CLOUD SEEDING PROGRAM <br /> <br />November 2002 started out with a continuation of the wet weather trend started during the second half of October. <br />Six weather systems over thirteen calendar days continued to maintain the above normal snowpack left by <br />Octobers weather systems. Early indications were that this winter might be near or slightly above normal for <br />snowpack and precipitation and allowed for earlier openings for most of the ski areas in Colorado. <br /> <br />The trend of frequent weather systems moving through the Western U.S. increased through December bringing <br />with it the occurrence of nine seeding opportunities over 21 calendar days into January 1, 2003. A subtle change <br />was becoming apparent with these systems. The intensity and duration of each system was becoming slightly less <br />as there was less southwesterly wind to bring in large amounts of moisture and most of the precipitation with these <br />systems was occurring mainly in the higher elevations ofthe mountains. By the end of December, the snow pack <br />in the Central Mountains had decreased to an average slightly under normal with several sites in the Seeding Area <br />continuing tu I", no "buve normal I ""diu!;;.. - . - - - - - . . - . - -. - .,- <br /> <br />The gradual drying trend of the weather system continued throughout January with shorter storm duration's for <br />seeding operations. Six seeding opportunities occurred over 12 days in January. At the end of January, the high <br />country snow pack in the Central Mountains had dropped to near 80% of normaL Most of the Seeded Area <br />monitoring sites still indicating ail additional 15% greater snowpack and precipitation. At the end of January, the <br />Vail region had received about 95% of its normal winter precipitation. <br /> <br />During the 2002-2003 Operational Seeding Program, all of the estimated seeding hours were utilized for the Vail <br />and Beaver Creek Ski Areas. Additional seeding hours were authorized when seeding opportunities existed during <br />the last half ofJanuary when Vail and Beaver Creek's cost portion of the Seeding Program ended for this season. <br /> <br />The Vail/Beaver Creek Operational Seeding Summary indicates the dates of all of this season's seeding operations, <br />the number of and total seeding hours of the generators in the network that were used to seed the ski areas, the <br />other generators in the network that were utilized or shared with the Vail/BC Program by the Denver or Upper <br />Arkansas Program and their operating hours and the Total Output of Silver Iodide for each operation for the <br />Vail/Beaver Creek Program., <br /> <br />The Seeding Program over the Vail and Beaver Creek Ski areas was continued by the sponsors of the Denver <br />Water Department Seeding program as the downwind seeding increases from this Program were beneficial to the <br />adjacent and downwind Denver Seeding Program Area. <br /> <br />Above normal precipitation and frequent weather systems with good seeding potential returned to the Central and <br />Northern Colorado Mountains during February with 8 weather systems and 21 operational seeding days. Februarys <br />snowpack increased so rapidly in the last half of February that an avalanche warning was issued. The average <br />precipitation for the region had increased to about 90% of normal with many monitoring sites in the Seeded Areas <br />indicating 10 to 15% more precipitation than adjacent unseeded sites. <br /> <br />The wet weather trend continued into early March and then quickly turned very dry with warming temperatures. <br />A very large slow-moving weather system moved into Colorado from the Southern California region in mid March <br />and produced nearly continuous precipitation for about six days. This one system produced nearly half of the <br />normal annual snowpack for the Eastern Slopes of Colorado and added about 10 to 15% to the spowpack in the <br />central Rocky Mountain Region. A second weather system moved into Colorado from the northwest a few days <br />later and contin~ed the mouf'kain ?re<;,1.?1.w.tion for another foor <!.a,s until the 11th of March. Se'ieral a'ialanche <br />warnings were issued for the Northern, Central and the East-slope Mountain Ranges in Colorado during these <br />