2014
DOI: 10.1007/s10546-014-9924-4
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Effects of Snowfall on Drifting Snow and Wind Structure Near a Surface

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Cited by 9 publications
(5 citation statements)
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“…However, during the measurement of the wind profile (Figure 1f), the fresh snow was not moving, thus not altering z 0 [39]. When snow is moving across the surface, this has been observed to increase the roughness [27,32,39]. In nature, snow grains fragment as they move across the surface [40]; thus, what is shown here is the initial movement of fresh snow (Figure 1e).…”
Section: Experiments and Implicationsmentioning
confidence: 90%
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“…However, during the measurement of the wind profile (Figure 1f), the fresh snow was not moving, thus not altering z 0 [39]. When snow is moving across the surface, this has been observed to increase the roughness [27,32,39]. In nature, snow grains fragment as they move across the surface [40]; thus, what is shown here is the initial movement of fresh snow (Figure 1e).…”
Section: Experiments and Implicationsmentioning
confidence: 90%
“…Dendrite-shaped snow crystals (Type A) were created at CES (see Figure 1 by Abe and Kosugi [26] and Figure 4 by Nemoto et al [27]). Using their technique, we also created these snow crystals in our experiment, which were then wind-blown across the surface of the bedforms (Figure 1e).…”
Section: Methodsmentioning
confidence: 99%
“…Airborne particles of sand or snow capture momentum from the air. When they strike the Earth, they launch further grains into the air (Anderson and Haff, 1988;Bagnold, 1941;Kobayashi, 1972;Schmidt, 1986). This process, known as saltation, is the primary method of momentum and energy transfer from the wind to a granular bed (Anderson and Haff, 1988;Schmidt, 1986).…”
Section: The Transport Of Loose Snow and The Erosion Of Solid Snowmentioning
confidence: 99%
“…When they strike the Earth, they launch further grains into the air (Anderson and Haff, 1988;Bagnold, 1941;Kobayashi, 1972;Schmidt, 1986). This process, known as saltation, is the primary method of momentum and energy transfer from the wind to a granular bed (Anderson and Haff, 1988;Schmidt, 1986). Saltation is initiated above a certain windspeed at which snow from the surface is entrained (Li and Pomeroy, 1997), and has considerable momentum thereafter.…”
Section: The Transport Of Loose Snow and The Erosion Of Solid Snowmentioning
confidence: 99%
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