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 6 years ago abgelaufen. Du siehst vergangene Verhältnisse, nicht den aktuellen Bericht.

Kernpunkte

Loose wet avalanches will be possible today in sun exposed areas during the late morning and afternoon hours due to weaker refreeze conditions and increased snow surface melt. MODERATE avalanche danger will exist today at all elevations.

Lawinenprobleme

  • Loose Wet

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

    Air temperature inversion conditions kept overnight lows well above freezing last night in most locations at the mid and upper elevations. Skies were clear so a decent, but likely superficial snow surface refreeze is expected to have occurred from radiational cooling of the snowpack last night. By the late morning hours, this surface refreeze will be gone in sun exposed areas and a loose wet avalanche problem will exist for the rest of the day. Avalanche size is expected mostly at D1 with up to size D2 possible in areas where the upper snowpack is less consolidated.

    Monitor snow surface melt throughout the day. The wetter and softer the upper snowpack becomes, the more likely it is for loose wet avalanches to occur. Once surface snow is more than a couple of inches deep, it’s time to exit avalanche terrain or move to an aspect with a firmer snow surface. Small loose wet avalanches could still have undesirable consequences in our relatively thin snow cover conditions as there are plenty of obstacles and hazards to hit.

Avalanche Discussion

* Observations made yesterday on Jake's Peak (West Shore Tahoe area) showed that increased warming and snow surface melt on mid and upper elevation E aspects created conditions more conducive to loose wet avalanches that what has occurred over the past couple of weeks. Despite all of the warm weather in recent weeks, there are many areas on E aspects where the upper portion of the snowpack has yet to become a consolidated, springtime melt-freeze snowpack.

* SE-S-SW aspects hold the most consolidated and well established melt-freeze snowpack conditions.

* NW-N-NE aspects remain highly variable, ranging from firm to soft with surface conditions ranging from ice to surface facets.

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