Abstract
The increase of the global radiation over a snow covered ground is an effect of the backscattering by the sky of the radiation reflected at the earth's surface. An attempt has been made to derive the coefficient of backscattering from observations both for clear and for overcast sky.
DOI: https://doi.org/10.3402/tellusa.v17i3.9069 | Journal eISSN: 3035-9554
Language: English
Page range: 350 - 355
Published on: Jan 1, 2012
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 2012 F. Möller, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.