Lawinenlagebericht

Central Sierra Nevada

Sierra Avalanche Center
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Lawinengefahr

Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
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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 continued snow surface melt. MODERATE avalanche danger will exist today at all elevations.

Lawinenprobleme

  • Loose Wet

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

    For two consecutive nights now, air temperature inversion conditions kept overnight lows well above freezing in most locations at the mid and upper elevations. Another superficial snow surface refreeze is expected to have occurred last night reliant on radiational cooling of the snowpack. Increasing cloud cover last night may have decreased the efficiency of radiational cooling, possibly creating a thinner refreeze than what existed yesterday morning. By the late morning to midday hours today, this surface refreeze will weaken and melt away 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 Mt. Judah (Donner Summit area) showed weak superficial snow surface refreeze on treed slopes and a stronger but still superficial refreeze on open slopes. Signs of a developing loose wet avalanche problem were present on SE-S aspects by midday.

* 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. This is increasingly prominent at the upper elevations. An observation received yesterday from Tamarack Peak (Mount Rose area) highlights this well.

* 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 (also highlighted in yesterday's Tamarack Peak observation).

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