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A Newsletter for Friends of the CAIC

A Newsletter for Friends of the CAIC

A Newsletter for Friends of the CAIC

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Powder Stashcontinued from page oneon December first, and we get an early start like we did this year?Until we find a way to work our budget to support <strong>the</strong> full season,we’ll be faced with this conundrum. Let’s hope this rash <strong>of</strong> accidentshas run its course. O<strong>the</strong>rwise, it will be a long winter.So on to better news, let’s turn to this issue <strong>of</strong> The Beacon.Included in this second issue <strong>of</strong> <strong>the</strong> season, are <strong>the</strong> usual widevariety <strong>of</strong> articles. We’re always looking <strong>for</strong> field data. We <strong>of</strong>tenget e:mail reports from friends and o<strong>the</strong>r backcountry travelersabout what <strong>the</strong>y saw on <strong>the</strong>ir days tour. We encourage <strong>the</strong>sereports, you are our eyes and ears in <strong>the</strong> mountains <strong>of</strong> Colorado.Andy Gleason has written a short piece on things that we reallylook <strong>for</strong> in <strong>the</strong>se reports. Timing is everything, if you can get usgood in<strong>for</strong>mation asap, we’ll put out a better product. It’s assimple as that.Last year <strong>the</strong> San Juan Mountains saw a couple <strong>of</strong> back to backstorm and avalanche cycles <strong>of</strong> near historical impact. OurSilverton intern, Susan Hale was <strong>the</strong>re and has written a personalaccount <strong>of</strong> <strong>the</strong> experience. It’s a hard article to put down. We’vealso included a short bio on our newest <strong>for</strong>ecaster (from last year),Spencer Logan. He’s got a pretty impressive resume, and eventhough he’s not that old in years, <strong>the</strong>re’s a chance he’s shoveledmore snowpits than all <strong>of</strong> us combined.Finally, Knox submitted a remembrance <strong>of</strong> a woman I had <strong>the</strong>good luck to have met on a couple <strong>of</strong> occasions, Sue Ferguson.Sue died last December from cancer. She lost her long fight withthis terrible disease, and even though we all knew she faced avery difficult battle, we were all greatly saddened by her passing.Both Sue and I shared a great love <strong>of</strong> glaciers, and <strong>for</strong>tunately,she left a legacy <strong>of</strong> avalanche research and glacier knowledgethat we will always be able to review. So put those snow shovelsaway <strong>for</strong> a bit, sit down and take a load <strong>of</strong>f, and enjoy yourBeacon. !BackcountryObservationsby Andy Gleason, Forecaster, <strong>CAIC</strong>-BoulderIn Colorado, we issue avalanche <strong>for</strong>ecasts from a central locationin Boulder. We rely on accurate and timely observationsfrom a network <strong>of</strong> backcountry and ski area observers. Weintegrate <strong>the</strong> observations that come into <strong>the</strong> Boulder <strong>of</strong>fice toproduce an avalanche <strong>for</strong>ecast <strong>for</strong> <strong>the</strong> entire state <strong>of</strong> Colorado. Ifyou, as a backcountry user, can send us observations about <strong>the</strong>snowpack and wea<strong>the</strong>r in your area, it can only help us create abetter <strong>for</strong>ecast and help to prevent avalanche accidents. Folkshave asked us if we want observations from “Lay-skiers”. Theanswer is an enthusiastic YES! The more observations we receive,<strong>the</strong> better in<strong>for</strong>mation we can include in <strong>the</strong> <strong>for</strong>ecasts. Don’tworry if your particular observation is not on <strong>the</strong> hotline, restassured it was still used to create <strong>the</strong> <strong>for</strong>ecast.The best way to send in your in<strong>for</strong>mation is via email atcaic@qwest.net. You can also call in your observations at 303-499-9650. The following are a few guidelines <strong>for</strong> observationsthat will help us make better <strong>for</strong>ecasts.Avalanche ObservationsThese are observations <strong>of</strong> recent avalanches that you have seenor triggered. Timing is everything. Old avalanche data helps fillour data base, but it’s <strong>the</strong> recent activity we need to broadcast. Ifyou see activity, let us know as soon as you can. The key points inavalanche reports are location, aspect, elevation, and slope angle.If <strong>the</strong>re are multiple avalanches, estimate <strong>the</strong> number you’veseen. The size <strong>of</strong> <strong>the</strong> fracture line, and width and length <strong>of</strong> <strong>the</strong>avalanches help us out, but are difficult to estimate from long distances.If you are familiar with avalanche classification, you cansend us a coded avalanche observation. If you would like to learnmore about how to describe avalanches check out <strong>the</strong> new Snow,Wea<strong>the</strong>r, and Avalanches: Observational Guidelines (SWAG) <strong>for</strong>Avalanche Programs in <strong>the</strong> United States, a publication <strong>of</strong> <strong>the</strong>American Avalanche Association (AAA). You can read <strong>the</strong> SWAGon <strong>the</strong> AAA website at http://www.avalanche.org/~research/guidelines/.Snowpack ObservationsThese include snow observations that help a <strong>for</strong>ecaster sittingin Boulder to get a clear picture <strong>of</strong> how <strong>the</strong> snowpack is reactingin your area. Things to include: shooting cracks, collapses,whumphs, ski or foot penetration, wind slabs, wind loading andwet snow. Please also include <strong>the</strong> location, aspect, elevation, andslope angle <strong>of</strong> where you were.Snow pits should be representative <strong>of</strong> avalanche starting zonesin <strong>the</strong> area, but should be dug in safe areas. Snow pits are great,but if you didn’t write up a <strong>for</strong>mal pit, let us know how deep it isto a specific weak layer. If you notice a prominent and persistentweak layer, report <strong>the</strong> depth from <strong>the</strong> surface, <strong>the</strong> type <strong>of</strong> snowabove it and <strong>the</strong> aerial extent. What are <strong>the</strong> snow surface conditions?They may not be contributing to <strong>the</strong> hazard now, but howwill new snow bond to <strong>the</strong> surface snow? Is <strong>the</strong> surface wet, dry,faceted, wind slab, ice-crust, or low-density powder?Any observations you make such as shooting cracks, collapses,whumpfs etc… should include <strong>the</strong> location <strong>of</strong> <strong>the</strong>se observationswith aspect, elevation and slope angle. Include pertinent negativessuch as no cracking or no movement on steep slopes too. Ifyou report a stability test, be sure to include what kind <strong>of</strong> test youconducted, <strong>the</strong> aspect, elevation and slope angle. You can alsoinclude shear quality in<strong>for</strong>mation.Here’s an example <strong>of</strong> a good concise report:Jill Outabounds, 12-21-05, 11:30 am. It is 22 degrees F with aSW wind at 10–20 mph. It has been snowing moderately (S1) <strong>for</strong>2 hours. I saw a HS-N-R2-D2-S on a NE, 32-degree slope at12,400’ in <strong>the</strong> San Juan range on Mt. Abrams. Fracture line 2–4ft deep, width 300’, vertical fall 1200’. The slope was wind loadedwith about 2 feet <strong>of</strong> new snow. We had shooting cracks andwhumpfing on NE to NW slopes between 10,000 and 11,500’.South facing slopes were wind scoured. A hasty pit on a NE, 27degree slope at 11,000’ showed surface hoar at a depth <strong>of</strong> 15”below new wind loaded snow. A compression test had CT-11 at15”, Q-1. No o<strong>the</strong>r failures in a snowpack 5’ deep. We skiedlower angle slopes on a north aspect and had good riding withsnowboard penetration <strong>of</strong> about 1 foot.If you want, feel free to tell us just how good <strong>the</strong> riding reallywas. We promise not to get too jealous. !2The Beacon, Winter 2006 ! Volume 10, Number 2

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