Good morning, this is Sue Burak with the Inyo National Forest Eastern Sierra Avalanche Center. Today is Tuesday February 24, 2009. MOUNTAIN WEATHER Enjoy the sun today because clouds and unsettled weather return mid week with another storm forecasted for the end of the weekend. Mountain areas above 8,000 ft will see southwest winds decrease today with gusts around 30 mph. Highs will be in the low 40s with lows around 20-25F. Elevations above 10,000 ft will see stronger southwest winds today gusting to 45 mph. High temperatures will be in the upper teens and low 20s. SNOWPACK AND AVALANCHE DISCUSSION For today, there are two very important avalanche concerns, wind loading and the persistent weak layers on the ground and the rain layer from January 22. These two avalanche problems can both be present and work in combination to great large avalanches. The wet Sunday/Monday storm added a significant load to the snowpack. A wind loaded slab avalanche released yesterday near the top of Carson Peak in June Lake. The slide ran more than 1,500 feet down the entire distance of Devils Slide. Though the initial slab up high in the bowl was small, the avalanche entrained dry and wet snow along the way that released on the weak snow on the ground. There are 8 ft debris piles at the bottom of Devils Slide. Above treeline and in exposed areas at treeline, the most likely place to trigger an avalanche is where new snow has been transported by the wind and formed into wind slabs. These will be found on north through east aspects. You can spot potential windslab conditions by looking for evidence of snow drifting: streaks on the snow surface; plumes of snow blowing off ridges; cornices forming; or if you are on the slope itself, feeling denser snow that may start to crack in front of you. Seeing any of these signs, especially if you also see recent avalanche activity, means it's time to back off onto less steep smaller slopes with safe zones that aren't exposed from above. Choose relatively low angle, uniform slopes with options for reducing risk. Avoid traveling in or above terrain traps where getting caught in a fairly small avalanche could have serious consequences. Smart, snow savvy people realize this is a very different snowpack this year from the forgiving Sierra snowpack of the past. The deeply buried facet layer and January rain layer remain reactive and are not going away. The buried weak snow has created a very unpredictable snowpack. The persistent charger attitude that the snowpack is bomber should be replaced with a healthy Rocky Mountain skepticism, especially with slopes that have not avalanched. Just because the snowpack is deep does not mean weak layers are exempt from loading from skiers and riders on the surface. There have been recent, natural large avalanches running in deeper snowpacks. Take an avalanche class to learn more about how to travel safely in the mountains. BOTTOM LINE In alpine terrain, the avalanche danger is estimated to be CONSIDERABLE above treeline on all north to east facing wind loaded slopes. Natural avalanches are possible. Variable conditions and uncertainty require conservative decision making. Careful route selection and good travel habits are required. The greatest danger exists on steep north to east facing wind loaded slopes from Rock Creek north to the Tioga Pass area. Terrain that is not wind loaded still has localized areas where an avalanche could be triggered. Avoid convex rollovers in steep trees and glades. The avalanche danger in no wind loaded terrain is MODERATE. In the Rock Creek and Bishop Creek area, the avalanche danger is estimated to be MODERATE above 8,000 ft. With less new snow and rain in this area, the buried weak layer remains active and many small slab avalanches were running on the buried weak layers yesterday. Please note that the avalanche danger rating in this advisory expires in 24 hours. This advisory is our best interpretation of snow pack conditions and NWS forecasts issued today. Backcountry travelers should be aware that elevation and geographic distinctions are approximate and that a transition zone exists between upper and lower elevations. Avalanches do not happen by accident and most human involvement is a matter of choice not chance. Most avalanche accidents are caused by slab avalanches that are triggered by the victim of member of the victim's party. Even small slides can be dangerous. Always practice route finding skills and carry avalanche rescue gear. Remember that avalanche danger ratings are only general guidelines. Distinctions between geographic areas, elevations, slope aspects and slope angles should be made.