Two Thumbs — Лавинный прогноз

We have no reports of any natural or human triggered avalanches in the last 2 days. Wednesday 29 July was actually less windy than forecast. Very little snow transport has been reported from guides and ski fields in the range and therefore no new windslab has developed . Although, some greenhousing was reported, it did not break the surface crusts and overall snow surface temperatures stayed relatively cold for the entire day.  If you see any activity on the Two Thumb Range, please make a public observation.  It really helps us to produce accurate forecasts. Rain, heavy at times about the Divide, spreading elsewhere from afternoon. Snow lowering to 1200 metres. The rain and snow amounts for tomorrow are forecast to taper from the North to the South. There is high uncertainty of the precipitation amounts. Some models predict 20cm around Stag Saddle and 5-10cm at Mount Dobson. Winds are forecast to be gale-force northwesterly 80 km/h, rising to severe gale 120 km/h for a time late morning to early evening.The free air freezing level starts out at 2200m in the South, but 1800m closer to the Divide. During the day it will be lowering to 1700m in the South (that is approx the car park of the Mount Dobson ski field),  but 1400m about the Divide in the evening. Firm surfaces exist, so be prepared for a possible sliding danger and assess each slope.  However, the incoming storm will soften the surfaces, either with some rain at lower elevation and in the morning, then later with some new snow.  Ski crampons should be in the pack! We do not think ice axe and crampons are essential with the weather forecast - you may want to avoid exposed ridges and summits tomorrow.

The snow depth in the range South of Stag Saddle is 40-60cm with some deeper pockets of 100-120cm in sheltered areas. The Two Thumbs still have good snow cover to elevations around 1100m.  The dry snow that fell throughout the range on Friday and Saturday has been redistributed by strong then moderate southwest and west winds at higher elevations.  Windward ridges are stripped with loaded areas up to 50cm deep.  Even at lower elevations, katabatic (cold air falling down the mountain) winds caused by the cold overnight temperatures, have moved the surface snow around. However, in the sheltered higher bowls in the centre of the range on the Eastern half, 5-15cm of dry none-wind affected snow is still present down to 1600m. The snowpack below the surface is capped by a crust of several layers that is highly variable over the terrain. In places it is thin and breakable with skis and in other places it forms large areas of solid concrete-like patches. Under the crust layers the snowpack is well consolidated.  Guides and ski fields have reported some sugary weak layers developing around the crusts. At present, this does not seem a problem in the South of the range. The snowpack North of Stag Saddle is not well understood, with no direct observations.  It is possible that above about 2300m very deep snow has accumulated.