[MCR] Bow -Peyto

3 days up at Bow and Peyto. In on the 28th, -3 in parking lot, good
travel, still solid by 1pm at hut.
29th over to Peyto.. +1.5 at Bow at 0700 soft heading up. Numerous
squalls and intermittent sleet and snow. By evening numerous point
releases on all aspects to size 1.5. On Rhonda N the steep snow
slope facing Peyto was sluffing all afternoon.
Isothermal conditions in pm most places off the glacier.

Peyto lake looked bluish...probably done for the year... I know from
descending it a week a go it was already getting sketchy in the
moraines for snow.

~ 5-10cm HN overnight then-3 at Peyto. April 3oth- Good travelling on
glacier back to Bow.

Numerous size 1-2's on moraines below and facing Bow Hut. Some others
closer to the turnoff to Crowfoot as well. Point releases stepping
down. Also on E facing slopes below Bow Bump there was a large size 2
out of the rocks. (All released on the 29th)

By 1130am getting isothermal on descent trail right from hut. had to
stay right on the track. (Lots of craters for those who didn't)

Some of the snow bridges in canyon have broken, not a big deal though.
Bow lake was still fine, down to ice but Ok when surface is soft.
Needs some cooler temps to glue this place back together.
Still suspect deep instabilities and caution as the warm temps have
deeply penetrated the snow pack and a significant cooling trend is
need to increase stability.
Peter

Peter Amann
Mountain Guiding
Box 1495, Jasper AB, T0E 1E0
www.incentre.net/pamann
pamann@incentre.net

_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.

[MCR] Hudson Bay Mountain 26 Apr 06

>>From the last field trip above my mining project, here is a report on the
conditions we found. Temperatures were -5.5 at 1900 m at 0900 with strong
southerly winds and light snowfall. Surfaces were very hard which made for
marginal travelling even with ski crampons on and heels down. We dug a pit
that showed rising snow temperatures - just a bit warmer than -2 for most of
the 150 cm - with a strongly frozen lid on top. We found hard shears 8 cm and
85 cm down in a snowpack that alternates between hard crusts and finger hard
facetted layers. We experienced one whumpf in a shallow snowpack area at 1600
m and saw no new avalanches. Skiing quality was fair at best.

--
Christoph Dietzfelbinger, Mountain Guide
Bear Mountaineering and the Burnie Glacier Chalet
Box 4222 Smithers B.C. Canada V0J 2N0
info@bearmountaineering.ca www.bearmountaineering.ca
tel. 250-847-3351 fax 250-847-2854

_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.

[MCR] Cirque pk/ Saddle mtn.

Saddle Mtn in Lk. Louise yesterday. Skied the N face couloir. Not quite yet
ready for good ski quality as the 3cm surface melt freeze crust made for
good traveling but poor skiing. Found the March SH (surface hoar) layer
(3-5mm 70% of it still standing proud) with a N facing, 20deg. test profile
@ 7700ft, 50cm down with easy compression/shear test. Would not have
continued to the couloir if it had not already slid recently. On the way
back from the Parkway today I noticed that the North Face of Saddle had slid
near ridge top in the last 12hrs, with a size 2 that surely slid on SH
triggered by pm warming. On this short fun tour, there is some route-finding
and steep boot packing down North side of ridge where it peters out into
steep cliffs- find inukshuk 40 meters down off ridge for gully feature
leading to top of couloir.

Cirque Pk today: Up the S ridge via Helen lake, thence down the SSE face
from summit. In perfect condition right now, with a short boot pack near
summit. Amazing long dist. vistas of Assiniboine, Bryce, etc. On this East
side of the highway the S aspects we skied were excellent. The corn is not
quite ripe yet but the cooler temps of Fri and Sat dried out the S asp snow
pack and created surface melt freeze re-crystallization that felt like a
skiff of powder up high and warmed to corn like snow below. No surface hoar
found, no whumfing or avalanches observed. Though it was a scorcher today,
due to the good overnight freeze we hardly got any snowballing or pinwheels,
neither was there any isothermal snow until below tree-line. Stability and
hazard definitely felt good up there today but if it really warms up as it
is forecasted beware of wet snow, isothermal slides on steeper aspects.
Get out there!
Eric Dumerac, Ass. Ski/Alpine Guide.

_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.

[MCR] Hudson Bay Mountain 20 Apr 06

Skied to the 1500 m observation site on the E side of Hudson Bay Mountain this
morning. The winds of the last two days did not bring much new snow. We could
see our old tracks in the big traverse at 1900 m, with some new snow in
deposition areas. Only one size 2 moist avalanche, cornice triggered, had run
between 1800 and 1400 m in the main path. We did not see any other new
activity. A profile in a sunny aspect at 1500 m showed an isothermal snowpack
with one shear 90 cm down. I don't think that the snowpack is isothermal in
higher and shadier locations yet.

--
Christoph Dietzfelbinger, Mountain Guide
Bear Mountaineering and the Burnie Glacier Chalet
Box 4222 Smithers B.C. Canada V0J 2N0
info@bearmountaineering.ca www.bearmountaineering.ca
tel. 250-847-3351 fax 250-847-2854

_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.

[MCR] Bow Hut, Mount Gordon

With all the negative factors affecting the Rockies’ snow pack right now (lots of recent new snow with strong winds, day-time warming with intense radiation, buried surface hoar layer lingering) decision making for day trips isn’t all that easy right now. Yesterday, I decided for a day trip to Mount Gordon along the Wapta Icefield.

 

Snow coverage on the approach to Bow Hut is good, including the Canyon. Cold temps especially in the morning (-14C at Bow Lake at 8AM) and about 40-50cm of settled new snow on the glacier made for ski penetration of roughly 10cm – 15 cm. There is evidence of intense wind transport from previous days, predominantly from south/westerly directions, which continued throughout the day along the ridgelines yesterday. Lots of really fat looking wind pillows lingering on slopes close to ridge lines.

 

Also, there have been a good number of recent avalanches, the largest (probably size 2.5 / 3) we saw was on Balfour Glacier. The start zone is in relatively low angle terrain on the glacier climber’s left (south) of the lower ramp commonly used to get to Balfour High Col and it ran into the Hector Lake approach to the Scott Duncan Hut. I suspect the slide was caused by the recent wind loading, possibly combined with the surface hoar layer prevalent on northern aspects in higher elevations along the Wapta Icefields. This surface hoar layer is currently buried 40 – 60cm deep and with wind-stiffened slabs above, many slopes could be prime candidates for skier triggering.

 

Enjoy the sunshine and stay safe!

 

Jorg Wilz

Mountain Guide (IFMGA / UIAGM)

 

www.ontopmountaineering.com

1-800 506 7177 or (001) 403 678 2717

 

[MCR] Howsons 13 to 17 April 06

Cool temperatures and 5 to 35 cm of storm snow (depending on elevation)
made for exceptional stability and skiing conditions. Ski crampons would
have made life a lot easier. Night time temperatures at the lodge
dropped to -9 and stayed about 2.5 during the day. I measured a 35 cm
thick crust in the morning, with the temperature 10 cm down at -6. There
are 118 cm of snow at the lodge and over 4 m on the glaciers. Crevasses
and creeks are very well bridged. Rotten snow was not a concern at all
and the corn skiing was excellent. Powder was to be found in cold
aspects and at elevations over 1800 m. The wind effect was not
interfering with the skiing very much. Mountaintop temperatures were
from -9 to -11 in mid-day, with moderate to strong west to southwest
winds. The only new avalanches were two size 2 slabs, triggered in steep
terrain by icefall, that consisted mostly of ice and some of the storm snow.
--
Christoph Dietzfelbinger
Mountain Guide, Bear Mountaineering and Burnie Glacier Chalet
Box 4222
Smithers, B.C. V0J 2N0 Canada
tel. 250-847-3351 fax: 250-847-2854
info@bearmountaineering.ca www.bearmountaineering.ca
_______________________________________________
These observations and opinions are those of the person who submitted them. The ACMG and its members take no responsibility for errors, omissions, or lapses in continuity. Conditions differ greatly over time and space due to the variable nature of mountain weather and terrain. Application of this information provides no guarantee of increased safety. Do not use the Mountain Conditions Report as the sole factor in planning trips or making decisions in the field.
Please check out http://acmg.ca/mcr for more information.

[MCR] Selkirk Mountains April 15/06 - back to winter

 

Just out from a week at Selkirk Lodge (halfway between Rogers Pass and Revelstoke), where conditions went from full spring corn/powder to a midwinter snowpack over the space of three days.

 

Currently an impressive spring storm has deposited between 40-60 cm. of snow in the last 48hrs. at Treeline elevations and likely closer to a meter in the high alpine – we observed snowfall rates yesterday afternoon in excess of 3 cm/hour that continued well into the night – moderate to strong winds from the SW accompanied this snowfall until they switched to moderate to strong from the North last night. This was followed by a dramatic cooling overnight (Friday April 14^th) with morning temps of -10 Celsius Saturday morning which seemed to help with the bonding of the storm snow to the crust below it.

 

We ski cut several steep rolls to test them with no results and other test results were likewise favorable – however when the skies cleared this afternoon while we waited for the helicopter to arrive we observed that the entire head of the valley (an exposed alpine cirque)  had released sometime late in the storm propagating over a distance of 2 kilometers and involving the release of terrain that was in the 25 degree incline – though much of it was steeper than that – aspect ranged from NE through NW – visibility was still foggy but it seemed to be several large slabs that I am highly suspect released simultaneously but that had small pieces of terrain still intact between them – anyway quite an event for sure and quite contradictory to our evidence a few kilometers away (and also several hours of time different).

 

All that to say that conditions have changed significantly in the mountains and special attention should be paid to the affects of daytime heating and the still lurking presence of the late March buried surface hoar layer in the high north facing alpine.

 

Cheers,

 

 

Scott Davis

Mountain Guide

 

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