Snowfall accumulations have not been sufficient to create an avalanche problem below treeline where the snowpack sits at about 30-60cms. Regardless, slopes at higher elevations have been large enough to run down to terrain located well below treeleine. In the alpine, and at treeline the snowpack depth generally sits anywhere from 80-120cm with deposits of up to 400 cms on wind-loaded features.Although not widespread, reports suggest that strong to extreme winds in some parts of the region have stripped west aspects of snow creating wind slabs on lee and cross-loaded aspects in the alpine and at treeline. Many of these new windslabs could be sitting on the reactive October rain crust located a few centimetres above the ground. This rain crust may have weak, overlying facets and is widespread in the alpine and isolated in its distribution at treeline in some parts of the region and non-existent in others.The 'take home' message is that the region as a whole is data-sparse and extremely variable in terms of snowpack structure. When heading into avalanche terrain, do so gradually and take the time to gather terrain-specific information. Any reports from the field are highly valued. Any observations can be sent to:
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