Geometry and Density of Drifts Formed by Snow Fences
Open Access
- 1 January 1980
- journal article
- research article
- Published by Cambridge University Press (CUP) in Journal of Glaciology
- Vol. 26 (94) , 405-419
- https://doi.org/10.1017/s0022143000010935
Abstract
This paper presents results from studies of snow-drifts formed by vertical-slat “Canadian” and horizontal-slat “Wyoming” snow fences having 50% porosity and heightsHfrom 0.8 to 3.8 m, on nearly level terrain. Characteristics of equilibrium lee drifts behind the Wyoming fence include cross-sectional area 19.3H2, length 30H, maximum depth 1.20H. and water-equivalent volume 6.8H2.18. Up-wind drift dimensions include maximum depth 0.5Hand length 12H. Drifts behind Canadian fences are about 25% smaller than for the Wyoming design. Polynomial regression equations are fitted to drift profiles for both fence types. Relationships are presented for the effects of wind orientation and curvature of drifts near fence ends, as well as empirical equations describing pre-equilibrium geometry relative to degree of saturation. Mean density ρ (kg/m3) of drifted snow having depthy(m), is given by ρ = 376+158 logy.Keywords
This publication has 2 references indexed in Scilit:
- Self-Similarity of Wind Profiles in Blowing Snow Allows Outdoor ModelingJournal of Glaciology, 1980
- The Shape of DrumlinsJournal of Glaciology, 1959