Good morning, this is Sue Burak with the Eastern Sierra Avalanche Center with an avalanche advisory posted on Saturday, February 16, 2008. Tonight, Ned Bair from the UCSB Bren School and I will be hosting a Nerd Night at 6 PM at the Mammoth Community Water District. I will talk about teleconnections; how the weather and climate around the world is strongly linked to weather and climate in other places through atmospheric connections. The Madden Julian Oscillation, El Nino and La Nina will also be discussed. Ned will present his findings on Patterns of slab avalanche release on Mammoth Mountain, a presentation that is sure to challenge the nerdiest of snow nerds. MOUNTAIN WEATHER The wind storm of Wednesday moved south and east and created significant snow for the mountains east of Los Angeles as well as Flagstaff and central New Mexico. Friday's temperatures were 20-25 degrees F warmer than Thursday's with Bishop warming from 42 F on Thursday to 59 F on Friday afternoon. Todays mountain temperatures will climb a few more degrees and remain in the mid to the upper 40s. Night time temperatures have also warmed 15 to 20 F into the mid 20s in mountain locations above the inversion that keeps lows in Lee Vining, Crowley Lake and Toms Place in the low teens. North winds will calm down today with ridgetop gusts in the 30-40 mph range. A pattern change from dry to wet weather is expected mid week. After a couple of weak shortwaves break down the ridge, a strong mid latitude jet will bring a succession of wet storms into central California for Wednesday night through Friday SNOWPACK AND AVALANCHE DISCUSSION After two cold and windy days, snowpack temperatures in the upper 6 inches of the pack have cooled off to -6 to -14 C on north and east aspects above 9,000 ft. Mid pack temperatures are warmer- temperature gradients and the resulting vapor pressure gradients are conducive for faceting to occur in the upper 4- 6 inches of the pack and water vapor moves from areas of high concentration to areas of low concentration. Strong gradients are turning rounds to facets. This process will continue on high north and east aspects for the next day or so and do not pose a stability problem right now. This layer will have to be monitored to see if gradients lessen before the weather changes next week. In the meantime, clear night time skies and light winds are the perfect conditions for surface hoar formation. Look for the sparkly, feather like crystals on open slopes the next few mornings. With little, if any new snow falling Thursday, I found only a few isolated pockets of wind drifted snow below the ridge tops today. I did not see any point releases today on southern aspects but this will change as snow temperatures increase in the upper 4-6 inches of the snowpack. However, I do not anticipate widespread wet snow instability because light north winds are forecasted to continue and temperatures are not expected to reach the mid to upper 50s as they did during the first few days of the week. BOTTOM LINE The avalanche danger rating remains LOW. This is a good time to ski big lines if you are not picky about skiing good quality snow from top to bottom. Many ridge top approaches have been stripped bare by southwest and north winds and exposed slopes can be very firm. 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.