Living Snow Fence Case Study: Mountain Lake, MN

snow-covered field with high snow drifts in back

A problem area along Highway 30 in Cottonwood County 10 miles west of Darfur is managed by a 2000-foot linear planting of honeysuckle. This living snow fence is set back 300 feet from the north side of the highway to capture blowing snow before it becomes a problem for travelers.

Steps used to design a living snow fence given the climatological and topographic characteristics at this site:

  1. Identify the snowfall over the snow accumulation season (SAS).
  2. Determine the prevailing winter wind direction by looking at: prevailing wind direction for October–March and the direction of predominant snow transport.
  3. Determine fetch distance for this site.
  4. Identify the snow water equivalent (SWE).
  5. Calculate the mean seasonal snow transport, based on snowfall over the snow accumulation season (SAS).
  6. Calculate storage capacity, based on fence porosity and height.
  7. Determine the angle of the prevailing wind with the road.
  8. Run model to get proper setback distance for fence.

Case Study Results

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Case Study Results

1. Snowfall

Map displaying the the mean monthly snowfall total over the dates of the snow accumulation season from 1971-2000

It is necessary to find the mean snowfall in order to calculate the mean seasonal snow transport in a later step.

The snow accumulation season (SAS) is delimited by the dates when average air temperature reaches 0° C, as computed from mean monthly temperatures.

Snowfall over the SAS is the mean monthly snowfall total over the dates of the snow accumulation season.

The 1971–2000 mean snowfall over the SAS is found on the adjacent map. Mountain Lake is denoted by the star.

The mean snowfall for this case study is 28 inches, or 0.711 meters.

View the SAS section of the mean snowfall page for more information on how this map was made.

2. Wind Direction

Prevailing wind direction and the wind direction of greatest potential snow transport are needed to calculate the attack angle later.

The first table gives the prevailing wind direction for each of the winter months, and the overall prevailing winter wind direction, 320° or NW. See a degrees vs. cardinal direction table.

OctNovDecJanFebMarOct–Mar
330320320310320330320

The second table gives the potential snow transport (Qupot). The direction of greatest snow transport is 320°, or NW.

The prevailing wind direction in this case is therefore 320°, or NW.

DirectionQupot (kg/m)
10471
2045
30145
40253
50109
60404
70127
80145
90178
100151
110244
120486
130552
140920
150854
160495
170763
1801,593
1902,611
2002,009
2102,027
2201,398
230775
240371
250302
260715
270721
2801,087
2905,402
30010,415
31018,781
32026,911
33018,895
3403,635
3501217
360687
Total =105,892

3. Fetch Distance

The fetch distance is used later to calculate mean seasonal snow transport, a variable used to find the ideal snow fence setback.

Fetch can be described as the length of an area that is contributing to blowing snow to a downwind location (Tabler 1994). The upwind boundary may consist of a large ditch, tree line, or farmstead.

For the case study at Mountain Lake, the fetch distance is 700 meters.

diagram of trees, fetch distance and line where snow starts to accummulate

4. Snow Water Equivalent

Map of Minnesota showing daily average snow water equivalents, with Mountain Lake marked in the south central part of the state, which has higher (wetter) snowfalls than the north and western areas of the state.

The snow water equivalent is another piece of data used later to calculate mean seasonal snow transport.

Average snow water equivalent, or the water equivalent of freshly fallen snow, is shown on the map.

For the case study at Mountain Lake, the snow water equivalent is 0.09. This means that 10 inches of snow is equal to 0.9 inches of liquid precipitation.

View the main snow water equivalent page for more information on how this map was made.

5. Snow Transport

A map of Minnesota labeled "Relocation Coefficient"

Mean seasonal snow transport is calculated to determine the amount of snow the snow fence will need to contain.

The mean seasonal snow transport (Qt) is calculated using the formula below. The equation utilizes the fetch distance and snow water equivalent found in the previous two steps.

For the case study at Mountain Lake, the mean season snow transport (Qt) is 22.3 t/m.

Formula for Mean Seasonal Snow Transport

Qt = 1500(S)(SWE)(r)(1-0.14F/3000)

  • Qt = mean seasonal snow transport (t/m).
  • S = mean snowfall over SAS (m).
  • SWE = mean snow water equivalent.
  • r = relocation factor for Mountain Lake, 0.25, (see map on the right).
  • F = fetch distance in meters.

6. Snow Storage Capacity

The porosity of the snow fence determines fence's snow storage capacity.

The table below gives the porosity fraction for various snow fences and the resulting snow storage capacity (Qc). Qc is calculated using the formula below.

For the case study at Mountain Lake, the porosity for the planting of honeysuckle was 0.20. Assuming the honeysuckle height to be 8.5 feet (2.59 meters), the snow storage capacity was 41.2 t/m.

Type of Fence
Porosity
Solid Fence
0.0
Double Shrub Row
0.275
Structural Snow Fence
0.50
Single Deciduous Tree Row
0.70
6-8 Rows Standing Strips of Corn
0.50

Snow Storage Capacity Formula

Qc/H2.2 = (3 + 4P + 44P2 - 60P3)

  • Qc is snow storage capacity in t/m.
  • H is the fence height in meters.
  • P is the porosity percentage of the fence.

7. Attack Angle

The attack angle of the prevailing winter wind striking the road is used to determine the fence's setback.

The most important consideration for attack angle is the predominant direction of snow transport, or the prevailing direction of the greatest amount of snow transport.

In this case, the wind direction should be taken as 320°.

With an east-west highway, the attack angle of the wind striking the road is 60°.

Wind Variables

Wind DirectionDegrees
Prevailing winter wind direction (Oct-Mar)320°
Prevailing winter wind direction of snow transport320°
Wind direction used as attack angle320°
Diagram of prevailing wind at 320 degrees and attack angle of 60 degrees

8. Setback

The formula below uses the attack angle, fence height, and porosity to calculate the setback of the fence.

The setback calculated for this case study at Mountain Lake, MN, is 165 feet (50.2 meters).

Formula for Fence Setback

D = H (sina) (12 + 49P + 7P2 - 37P3)

  • D is the setback (m).
  • H is the height of the fence (m).
  • sina is the attack angle of the prevailing winter wind striking the road.
  • P is the porosity percentage of the fence.

Conclusions

snow-covered field with shrub snow fence in the center; higher drifts on right side of the fence

The observed snow storage was found to be 18.6 t/m at Mountain Lake. The storage capacity of this fence design is 41.2 t/m; therefore this design captured roughly 45 percent of capacity for the 2000–01 season.

The calculated setback distance of 165 feet is 135 feet greater than the actual setback of 300 feet. However, no problems occurred at this site because snow deposition did not encroach on the roadway.

References

Gullickson, Dan et al., 1999. Catching the Snow with Living Snow Fences. MnDOT Office of Environmental Services and University of Minnesota Extension Service (MI-7311-S), 140 pp.

Tabler, R.D., 1994. Design Guidelines for the Control of Blowing and Drifting Snow, Strategic Highway Research Program, Washington D.C., 364 pp.