Bollettino valanghe

Central Sierra Nevada

Sierra Avalanche Center
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Pericolo valanghe

Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
2 · Moderato
Non aggiornato — questo bollettino è scaduto 10 years ago. Stai vedendo condizioni passate, non il bollettino in corso.

In sintesi

MODERATE avalanche danger will form on sun exposed E-SE-S-SW-W aspects steeper than 35 degrees at all elevations as daytime warming creates wet snow on these aspects. Loose wet snow avalanches including roller balls, pinwheels, and point releases will be possible today. While cornice failure has become unlikely, it is not impossible and today's warming could also weaken some of the large overhanging cornices that exist on the NW-N-NE-E-SE aspects along exposed ridgelines on isolated terrain features as well. 

Problemi valanghivi

  • Glide Cracks

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely
    Dimensione
    3

    Many of the the large cornices that formed during the recent storm failed during or just after the storm and some have broken under the weight of a person or snowmobile since the storm. However, many large overhanging cornices still remain perched above wind loaded slopes along exposed ridgelines. While these cornices have become more difficult to break, today's warming will weaken these cornices, and the potential exists for some of them to break on isolated terrain features where they are most overhung and least supported. A great deal of uncertainty exists concerning the strength of these cornices and how far back they may break.

    Identify where cornices exist and stay well back from their edges. Often determining how much a cornice overhangs a slope is difficult, and even when the overhang is visible, they can break behind that point. Giving these large cornices more space than seems necessary represents a wise choice.

  • Loose Wet

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    2

    Even though temperatures remained above freezing in some areas last night, the clear skies allowed the snowpack to radiate heat out into the night sky and refreeze. This refreeze will quickly melt away as the strong March sun and warm daytime temperatures heat up the snowpack. The snowpack has not been through enough melt freeze cycles to form good drainage channels to deal with the free water that forms due to the warming or to transition to corn snow conditions. Once the refreeze melts, loose wet snow avalanches in the form of roller balls, pinwheels, and point releases will become possible again today. The sun exposed E-SE-S-SW-W aspects hold the best potential for loose wet avalanches. Most of the loose wet snow instabilities should remain small, but some of them could entrain enough snow to cause problems for backcountry travelers. 

    Use clues like sinking into boot-top deep wet snow and smaller surface wet snow instabilities like roller balls and pinwheels to indicate that enough wet snow exists for problematic loose wet avalanches. These signs indicate that the time has come to move to more frozen slopes, move to less steep slopes, and/or switch activities for the afternoon. 

Avalanche Discussion

Yesterday observations from Donner Peak, Mt. Judah (Donner Summit area), Jakes Peak, and Stevens Peak (Carson Pass area) all showed wet snow forming on the sun exposed aspects by mid morning. Human triggered roller balls and pinwheels occurred on Jakes Peak, Mt. Judah, and on Stevens Peak. On Donner Peak observers noted a glide crack had formed as the snow slowly slid down one of wet granite slabs. Also some natural loose wet activity started to occur on low elevation east facing slopes by 10 am. The north facing aspects also held wet snow and breakable crusts below 7800 ft. on Mt. Judah and below 8500 ft. on Stevens Peak. Above these elevations the north facing aspects held a mix of firm wind packed surfaces on exposed slopes and shallow cold soft snow on sheltered slopes. Large cornices still loomed over many slopes in the Mt. Judah area, along the Sierra Crest south of Mt. Judah, and in the Desolation Wilderness around Jakes Peak. 

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