Abstract
Summary The Meteorological Service of Canada and the Ontario Hydro-Electric Power Commission are conducting an International Hydrologic Decade study of ice formation and dissipation on the upper Niagara River. As a contribution to this project, an estimate of the energy balance of the river has been made, based on long term climatological data and on hydrological observations obtained during the 1967 ice season. This paper discusses the magnitudes of various terms in the energy balance equation and suggests applications of the energy budget approach to problems of ice forecasting.
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