Wind-blown Snow as a Water Resource
Basics of Blizzards and Snowdrift Control

Snow Transport
How much water forms the snowdrift behind a snow fence that trapped all the snow drifting off a fetch in a winter? Let's figure this out for each foot (or meter) of snow fence length (across the wind). Starting with the total winter's snowfall on the fetch, part is held by vegetation and blizzards sweep off the rest. Some of what blows evaporates, and what finally arrives at the fence we call snow transport. Usually we want the number for an average winter. This diagram shows the concept (after Tabler, 1975).

Fetch may be greater or less than the transport distance, in which an average-sized blizzard particle evaporates completely. In Wyoming (and in other regions), our studies show that transport distance is about 10,000 ft (3000 m). We estimate what evaporates by the ratio of fetch to transport distance.


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