For the first time an attempt is made to derive a theoretical relationship between sea-ice strength and the controlling factors of salinity, temperature, and density. A geometric model of the ice-brine relationship is constructed from photographs and used to calculate tensile strength of warm (above - 20°C) sea ice. The theoretical results compare well with experimental data. The model developed can be extended to colder temperatures by considering the effect of solid salts
In this thesis we investigate how supercooling in the ocean near an ice shelf affects the mass balan...
The freezing of water to ice is a classic problem in applied mathematics, involving the solution of ...
Ice formed from seawater, called sea ice, is both an important actor in and a sensitive indicator of...
The brine content of sea ice influences many of its properties like e.g. thermal conductivity, melti...
Preliminary results are reported of field studies 1955-56 by the U.S. Air Force Cambridge Research C...
The large-scale Arctic sea-ice retreat induces a gradual replacement of thick, multi-year sea ice by...
International audiencePure ice, brine and solid minerals are the main contributors to sea ice mass. ...
One method of thickening an ice sheet is "free flooding": ice is built up by successive flooding and...
A model of the thermo-elastic behaviour of saline ice is formulated, and model solutions describing ...
The freezing of sea water in polar regions has important implications for ocean circulation and henc...
The measured flexural strengths of freshwater ice and sea ice have been compiled with a view towards...
The work presents the study of changes in the physical and mechanical properties of sea ice in bendi...
The composition of impurities in ice controls the stability of liquid water and thus the distributio...
The salinity, density, and petrographic structure of sea ice grown in a confined system can be close...
In this thesis we investigate how supercooling in the ocean near an ice shelf affects the mass balan...
The freezing of water to ice is a classic problem in applied mathematics, involving the solution of ...
Ice formed from seawater, called sea ice, is both an important actor in and a sensitive indicator of...
The brine content of sea ice influences many of its properties like e.g. thermal conductivity, melti...
Preliminary results are reported of field studies 1955-56 by the U.S. Air Force Cambridge Research C...
The large-scale Arctic sea-ice retreat induces a gradual replacement of thick, multi-year sea ice by...
International audiencePure ice, brine and solid minerals are the main contributors to sea ice mass. ...
One method of thickening an ice sheet is "free flooding": ice is built up by successive flooding and...
A model of the thermo-elastic behaviour of saline ice is formulated, and model solutions describing ...
The freezing of sea water in polar regions has important implications for ocean circulation and henc...
The measured flexural strengths of freshwater ice and sea ice have been compiled with a view towards...
The work presents the study of changes in the physical and mechanical properties of sea ice in bendi...
The composition of impurities in ice controls the stability of liquid water and thus the distributio...
The salinity, density, and petrographic structure of sea ice grown in a confined system can be close...
In this thesis we investigate how supercooling in the ocean near an ice shelf affects the mass balan...
The freezing of water to ice is a classic problem in applied mathematics, involving the solution of ...
Ice formed from seawater, called sea ice, is both an important actor in and a sensitive indicator of...