Lawinenlagebericht

Central Sierra Nevada

Sierra Avalanche Center
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Lawinengefahr

Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
Veraltet — dieser Lagebericht ist 11 years ago abgelaufen. Du siehst vergangene Verhältnisse, nicht den aktuellen Bericht.

Kernpunkte

Early this morning, LOW avalanche danger exists for all elevations and aspects. Pockets of MODERATE avalanche danger will form quickly in response to daytime warming on E-SE-S-SW aspects at all elevations on slopes 35 degrees and steeper. On W-NW-N-NE aspects, avalanche danger will remain LOW. Isolated wind slabs may exist above treeline on S-SW-W-NW-N aspects, but are not expected to be a widespread avalanche problem today.

Lawinenprobleme

  • Loose Wet

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    2

    Air temperatures above 7,000' at 6 am this morning ranged from the upper 20s to mid 40s. In areas where air temperatures were at or above freezing, snow surface refreeze last night will have been entirely dependent on radiational cooling under clear skies. This superficial refreeze is expected to be a fairly thin in most areas and will melt quickly this morning.

    The snowpack on E-SE-S-SW aspects remains in a transitional state. Under the relatively weaker and lower angle early February sun, daily melt-freeze cycles have been insufficient to produce corn snow conditions. What exists instead is a few inches of surface wet snow on top of colder, dry, less consolidated remnant storm snow, sitting on top of rain crust.

    Once the thin ice layer of overnight snow surface refreeze is gone, marginally supportable conditions exist and the snowpack structure is conducive to human triggered loose wet avalanche activity. Snowpack failure has been occurring at the interface between the surface wet snow and the colder drier snow below it. In most areas this has manifested as human triggered roller balls and pinwheels. In more isolated areas human triggered loose wet avalanches large enough to bury or injure a person are possible in steep terrain. A few loose wet avalanches in recent days have been observed to entrain dry snow down to the rain crust, increasing the depth of debris piles.

    The problematic surface wet snow over drier, colder snow structure is easily identified by hand pits as this structure exists within the top 6 to 8 inches of the snowpack in the vast majority of areas on E-SE-S-SW aspects. In areas where this snowpack structure exists, avoid travel on slopes steeper than 35 degrees and stay out from under steeper terrain above.

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely
    Größe
    1

    Yesterday's stronger than forecast E winds were observed to transport snow in isolated areas above treeline. Some isolated small wind slabs may exist on S-SW-W-NW-N aspects today. This is not expected to be a widespread avalanche problem, but warrants some caution.

Avalanche Discussion

Observations made and received yesterday from Castle Peak and Andesite Ridge (Donner Summit area), Jakes Peak (West Shore Tahoe area), and Echo Peak (Echo Summit area) all revealed similar conditions. A poor overnight snow surface refreeze had occurred and surface wet snow was widespread on E-SE-S-SW aspects by mid morning. Signs of recent loose wet instability existed in most areas. Most instability had taken the form of roller balls and pinwheels. Small to medium size loose wet avalanches that had occurred over the past 5 days were noted in steeper terrain. The marginally supportable upper snowpack structure of wet snow over dry snow over rain crust was observed on E-SE-S-SW aspects in all of these areas. Snow depth above the rain crust ranged from 2 to 10 inches deep. Yesterday's E winds were reported to have scoured down to and exposed the Jan 29 rain crust in some areas on N-NE-E aspects near and above treeline.

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