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by evapotranspiration is greater than in cloudy and cool weather. The storm began to warm but it’s questionable if the snow could have bonded with the crust if the snow remained relatively cold and hard. The potential for direct-action avalanches would have been higher on south-facing slopes if the three feet of snow had accumulated faster or if the storm had been upside-down. Since the snow fell at relatively warm and consistent temperatures over the five-day period, it probably had time to settle and bond. The storm also finished right-side-up with slightly cooler The hottest product vintage book lovers reading jane austen book stack all over printed tote bagtemperatures and lower-density snow. In addition, the wind direction during the storm was not favorable for loading the south-facing slopes since they were actually windward at that time. However, the avalanche potential would certainly increase once the strong northerly winds transported the new snow back over the ridge and onto those south-facing slopes that had a good sliding surface below. High pressure, also called an anticyclone, occurs when descending air molecules “pile up” at the surface and spread outward in a clockwise rotation in the Northern Hemisphere . Descending air warms, which prevents water vapor to condense into clouds to produce storms. Instead,

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