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Ice-Cover Breakup and Ice Jamming
2019During the ice-cover period, initial ice-cover breakup precedes ice-jam flood events. Hence, it is important that breakup processes are well understood in order to be better prepared for ice-jam flood forecasting. Being able to predict ice-cover breakup provides an indication when ice-jam flood forecasting should commence.
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The choice of constitutive relations for an ice cover
Journal of Applied Mathematics and Mechanics, 1999The authors dwell on the rheological correlations between the internal stresses and the strain parameters of the sea ice cover. In this regard the AIDJEX model [see \textit{M. D. Coon, G. A. Maykut, R. S. Pritchard, D. A. Rothrock} and \textit{A. S. Thorndike}, AIDJEX Bull. 24, 1-105 (1975)] and the Hibler model [see \textit{W. D. Hibler III}, J. Phys.
Gol'dshtejn, R. V., Marchenko, A. V.
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2019
This chapter illustrates many techniques used to monitor the ice cover during the winter season, which are necessary to determine important characteristics of the ice cover. Such information is useful when making predictions concerning ice-cover breakup and ice-jamming potential at the end of the winter season.
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This chapter illustrates many techniques used to monitor the ice cover during the winter season, which are necessary to determine important characteristics of the ice cover. Such information is useful when making predictions concerning ice-cover breakup and ice-jamming potential at the end of the winter season.
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A model of a drifting ice cover
Journal of Applied Mathematics and Mechanics, 1994zbMATH Open Web Interface contents unavailable due to conflicting licenses.
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Deterioration of Floating Ice Covers
Journal of Energy Resources Technology, 1985The deterioration of floating ice covers is analyzed to determine under what conditions the ice cover loses strength due to internal melting. The analysis considers the interaction between sensible heat transfer and long wave radiation loss at the surface, the surface albedo, the short wave radiation penetration and absorption and the unsteady heat ...
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Hydrobiologia, 1996
Mixing in ice covered lakes is caused by through-flow currents, oscillations of the ice cover and by convective currents induced by heat flow from the sediments or by solar radiation penetrating the ice. Mainly from studies in Swedish lakes, current velocities and mixing coefficients are quantified for the different processes generating water movement.
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Mixing in ice covered lakes is caused by through-flow currents, oscillations of the ice cover and by convective currents induced by heat flow from the sediments or by solar radiation penetrating the ice. Mainly from studies in Swedish lakes, current velocities and mixing coefficients are quantified for the different processes generating water movement.
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The Decreasing Arctic Ice Cover
Physics Today, 2000Ongoing monitoring of Earth's north polar region has been turning up numerous signs of change in its atmosphere, waters, and ice pack (see PHYSICS TODAY, November 1998, page 17). Such studies have revealed that the Arctic ice mass is shrinking, but now, it seems, the rates of decline are much more rapid than previously thought.
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Changes in river ice cover in the context of climate change and dam impacts: a review
Aquatic Sciences, 2023Maksymilian Fuks
exaly