## Abstract Measurements were conducted in coniferous forests of differing density, insolation and latitude to test whether air temperatures are suitable surrogates for canopy temperature in estimating sub‐canopy longwave irradiance to snow. Air temperature generally was a good representation of ca
Dependence of snow melting and surface-atmosphere interactions on the forest structure
✍ Scribed by J. Otterman; K. Stáenz; K. I. Itten; G. Kukla
- Publisher
- Springer
- Year
- 1988
- Tongue
- English
- Weight
- 517 KB
- Volume
- 45
- Category
- Article
- ISSN
- 0006-8314
No coin nor oath required. For personal study only.
✦ Synopsis
The surface albedo and the surface roughness for forested areas with snow on the ground are expressed in terms of the tree silhouette parameter s, the projection on the vertical plane of trees per unit area. The absorption of insolation (direct solar beam) is quantitatively described for a horizontal snow surface with vertical tree trunks, stressing the role of the bark at snow level as triggering the snow melt.
Measurement of s by field sampling in two forested sites in central Switzerland yielded values ranging from 1.8 to 2.1.
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