Budyko, M. I. (1956). Teplovoi Balans Zemnoi Poverkhnosti. Leningrad:
Gidrometeorologicheskoe Izdatel'stvo. (English transl.: Stepanova, N. A. (1958). The Heat Balance of the Earth's Surface. Office of Technical Services, U.S. Dept. of Commerce, Washington, DC.) Geiger, R. (1959). The Climate near the Ground. Cambridge, MA: Harvard University Press.
Gray, D. M. and Male, D. H. (1981). Handbook of Snow. Toronto: Pergamon Press. Houghten, H. G. (1954). On the annual heat balance of the Northern Hemisphere. J. Meteorol., 11, 1-9.
Lamb, H. H. (1955). Two-way relationships between the snow or ice limit and 100-500 mb thickness in the overlying atmosphere. Q. J. Roy. Meteorol. Soc. 181, 172-189. Sverdrup, H. U. (1935). Scientific results of the Norwegian-Swedish Spitzbergen expedition in 1934. Part IV. The ablation on Isachsen's Plateau and on the 14th of July Glacier. Geogr. Ann., 17, 53-166. Wallen, C. C. (1949). Glacial-meteorological investigations on the Karsa Glacier in
Swedish Lappland 1942-1948. Geogr. Ann., 30, 451-672 Williams, J. (1975). The influence of snow cover on the atmospheric circulation and its role in climate change. J. Appl. Meteorol., 14, 137-152.
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Renewable energy is energy that is generated from sunlight, rain, tides, geothermal heat and wind. These sources are naturally and constantly replenished, which is why they are deemed as renewable. The usage of renewable energy sources is very important when considering the sustainability of the existing energy usage of the world. While there is currently an abundance of non-renewable energy sources, such as nuclear fuels, these energy sources are depleting. In addition to being a non-renewable supply, the non-renewable energy sources release emissions into the air, which has an adverse effect on the environment.