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freezing (-2 or -1°C) between 1800Z April 2 and 0000Z April 3. Then they fall to -5 or -6°C by 1200Z April 3. Actual instrument data had a maximum of 29°F (-2 °C) the afternoon of April 2 and a minimum of 22°F (-6 °C) at 1200Z on April 3. Surface hoar layers probably formed between storms when it was clear, especially on open slopes protected from the wind. Without snowpit test results to verify the depth and weakness/strength of these layers, our pre-season weather information leads us to treat the facets on the crust as the most likely weak layer to fail with any The hottest product i lived in books more than i lived anywhere else tote bagavalanches that might occur. We don’t know how deep the individual layers are, but most of the snowpack since late November has sat atop the ice crust and near-surface facet layer, which developed in late November and early December. Layers of surface hoar could also be interspersed with layers of near-surface facets higher up in the pack, which formed between the smaller storms from late December thru January. However, we do not know for sure. Remember to read the synopsis before moving on to the next case.
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