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Other expected effects include water scarcity in some regions and increased precipitation in others, changes in mountain snowpack, and adverse health effects from warmer temperatures.
Longwave radiation is received by the snowpack from many sources, including ozone, carbon dioxide, and water vapor present in all levels of the atmosphere.
Mountain hemlock is adapted to sites with long-lasting snowpacks.
If snowfall stays on the ground for a series of years uninterrupted, the snowpack develops into a mass of ice called glacier.
The average snowpack per year is 10.5 feet, with over 15 feet of snow depositing in certain areas.
High surface temperatures can intensify droughts by enhancing evapotranspiration in summer, and increasing sublimation and melting of the snowpack during winter.
Snowpacks are an important water resource that feed streams and rivers as they melt.
Variations in substrate, topography, moisture, and snowpack depth and duration determine the vegetation community.
The energy balance of the snowpack itself is dictated by several heat exchange processes.
This limitation of light transmission through the snowpack decreases light availability under the snow.
Skis and snow shoes are less likely to collapse subnivean space if the snowpack is deep enough.
It is important to note that some of these trails depend on sufficient snowpack.
Snowpack is the seasonal accumulation of slow-melting snow.
Decreased snowpack and earlier runoff will decrease stream flow.
The biggest factors determining the effects on electricity are annual temperature changes and the change in peak snowpack melt and stream flow.
