Eastern Sierra Avalanche Bulletin
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avalanche danger;
corn ;
low pressure;
rescue gear;
slab;
sluffing;
sluffs;
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Good morning, this is Sue Burak with the Inyo National Forests Eastern
Sierra Avalanche Centers advisory posted for the week of May 27 to May
30, 2008.
This is the final avalanche advisory for the season.
Mountain Weather
The unusually cool to cold windy weather will continue until the end of
this week. A massive low pressure system continues to rotate over
California, sending out shortwaves that keep the weather unsettled and
wet. Another upper shortwave rotates around the low over Mono County
this morning, with storms beginning by 11AM.
The upper low is moving slowly east but the emphasis is on the word
slow. Today will be a repeat of Tuesdays weather with early morning
clear skies followed by rain showers by late morning. Freezing levels
will be 9500 to 10,000 ft with possible snowfall in isolated areas near
convection cells. The unsettled weather continues Thursday with a brief
break on Friday.
Temperatures will be in the upper 30s at the 9,000 ft elevation and mid
30s at 10,000 ft. Higher elevations will see highs in the low to mid
30s for the next few days with lows in the 20s. Winds will be gusty
around the storms with south and southwest winds gusting to 25 mph. The
Owens Valley will have another windy day with gusty southerly winds in
the 20 to 30 mph range.
The long range forecast is for thunderstorms and rain/snow showers for
the weekend.
Snowpack and Avalanche Discussion
The downhill slide of snowpack loss has been temporarily and
delightfully postponed by the cold wintery weather of the last week.
The higher elevations of the eastern Sierra picked up 10 to 12 inches
of new snow. The Sonora Pass area picked up a foot of new with over an
inch of water. Bishop Pass picked up over an inch of water as did
Mammoth Pass and the high elevation Gem Pass. Calm to light winds and
cold temperatures made for a great day of skiing on Monday.
Wet slide activity increased yesterday with clear morning skies and
late May radiation. Not much new snow accumulated yesterday and not
much is expected for today. With the cold nights, the spring corn cycle
is renewed and there is enough snow to slow the progress of sunup
growth. The new snow is sluffing readily so position yourself and
others to avoid getting caught in large spring slides. Any new snow
will be more sensitive to the suns heating than older snow. Spring
temperatures and sunshine are intense and will initially decrease the
stability of any new snowfall on steeper slopes. Pay close attention to
how deep the overnight freezes penetrate the snowpack.
Avalanche danger during this period of cool and unsettled weather is
except on very isolated steep slopes with accumulations of fresh
snow. Late spring radiation will rapidly transform winter pow to turn
to sticky glop. After the new snow is melting, it doesnt take much time
for wet snow sluffs to occur. The avalanche danger can be in
these areas.
Bottom Line
Avalanche danger during this period of cool and unsettled weather is
except on very isolated steep slopes with accumulations of fresh
snow. Late spring radiation will rapidly transform winter pow to turn
to sticky glop. After the new snow is melting, it doesnt take much time
for wet snow sluffs to occur. The avalanche danger can be in
these areas.
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.
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