Avalanche Advisory Archive Pre-2016
| Date Issued: | 2011-02-28 |
|---|---|
| Danger: | 3 |
| Trend: | 3 |
| Probability: | 3 |
| Size: | 2 |
| Problem: | 0 |
| Discussion: | The National Weather Service Forecasts- TODAY...MOSTLY CLOUDY. LOCALLY VERY WINDY. HIGHS AROUND 16. TONIGHT...MOSTLY CLEAR. LOCALLY VERY WINDY. LOWS 3 TO 9. TUESDAY...PARTLY CLOUDY. LOCALLY VERY WINDY. HIGHS AROUND 16. TUESDAY NIGHT...PARTLY CLOUDY. LOCALLY WINDY. LOWS 1 TO 9. We have received 4-6\" of new snow on Friday night. Since that time there has been a great deal of blowing and drifting snow. This wind event is building slabs on our south and southwest facing slopes. These slabs have been easily skier triggered. Ranging from 4-10\" in thickness. Today we may see some natural activity at or near that same depth. As long as wind transport continues these slabs have the ability to grow and turn in to avalanches. The lower weak layers in place appear to be holding and gaining strength so we do not expect avalanches at a deeper level creating a larger size. There is still a possibility of deeper larger avalanches yet they are not predicted. Be safe if you head out into the backcountry. Remember Partner, Transceiver, Probe, Shovel. Choose good lines, make good decisions, and live to play another day! |
| Tip: | WINDS What direction the slope faces with respect to the wind is a HUGE factor. Yes, it's true! And this takes most people by surprise. But ignore wind at your own peril. It's easy to ignore wind too because we human beings are big and heavy creatures and most of the time, we hardly even notice wind unless it mess up our hair.But imagine yourself as a bird where wind is its entire world. Then imagine yourself as something even smaller and lighter--like a feather?or, how about new fallen snow? Wind to a delicate snowflake is like the ocean current to plankton. So why is wind important? As we have learned, loading (added weight) causes of most avalanches and the fastest way to load a slope is by wind. Wind erodes from the upwind side of an obstacle such as a ridge and it deposits on the downwind side, and wind can deposit snow ten times more rapidly than snow falling from the sky. Wind deposits snow most commonly on the leeward side of upper elevation prominent terrain features such as ridges, peaks and passes. We call this \"top loading.\" But wind can also blow across a slope which we call \"cross loading\" and wind can even cause loading when it blows down a slope. Remember that wind can blow from any direction and thus deposit snow on most any slope. The bottom line: be suspicious of any steep slope with recent deposits of wind drifted snow. Typical Wind Slab Locations: Ridgetop Loading: Ridge top winds transport wind from the windward side of a ridge to the lee slope. Cornices are often formed on steep ridgelines but may not be present on rounded ridge tops. Windward slopes may show scoured snow and or exposed rock or grass. Side Loading: Cross slope winds typically load gullies and chutes. This may occur at any elevation depending on winds. Higher areas will typically be scoured. Low areas may look smooth. Wind slabs are so dangerous because: ? As the wind bounces the eroded snow across the snow surface, it grinds up the snow into small, dense particles. By the time they finally come to a rest on lee of an obstacle--where the wind slows down--they pack into a heavy, dense layer of snow that can easily overload any buried weak layer. ? When strong wind starts to blow, within minutes, wind can turn nice fluffy powder into a dangerous wind slab. When very safe conditions quickly turn into very dangerous conditions, it easily takes people by surprise. ? Wind slabs can form in extremely localized areas. Often only a few inches separates safe snow from dangerous snow. We often hear people say, \"I was just walking along and suddenly the snow changed. It started cracking under my feet, and then the whole slope let loose.\" How to Recognize Wind Slabs: Lucky for us, wind creates easy-to-read textures on the snow surface and characteristically shaped deposits. No one should go into avalanche terrain without first learning how to read these obvious signs. An old avalanche hunter's adage: If you have developed a good eye for slope steepness and the effects of wind, you can avoid about 90 percent of all avalanches. Eroded snow vs. Deposited Snow Eroded snow: ? Looks Like: has a sandblasted, scoured, scalloped, roughed-up look. Deposited snow (wind slabs): ? Looks Like: smooth and rounded, lens shaped, pillow shaped, chalky-white color |
