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Abstract
Four processes are identified as determining the initial interception of falling snow by forest during storms: delivery of snow particles from the airstream to the forest; true throughfall of particles to the forest floor; impaction and adhesion of particles to foliage and branches; and cohesion of particles into masses of snow. Delivery and impaction processes seem amenable to aero-dynamic analysis; adhesion of particles and cohesion both depend on air temperature and foliage roughness. Promising leads for laboratory and field research on aerodynamic and thermodynamic factors influencing interception are described.
Citation
Miller, David H. 1964. Interception processes during snowstorms. Res. Paper PSW-RP-18. Berkeley, CA: Pacific Southwest Forest & Range Experiment Station, Forest Service, U. S. Department of Agriculture; 24 p