Add to ORKGA method to estimate the flexural stiffness and effective elastic modulus of floating ice is described and analysed. The method is based on the analysis of water pressure records at two or three locations below the bottom of floating ice when flexural-gravity waves propagate through the ice. The relative errors in the calculations of the ice flexural stiffness and the water depth are analysed. The method is tested using data from field measurements in Tempelfjorden, Svalbard, where flexural-gravity waves were excited by an icefall at the front of the outflow glacier Tunabreen in February 2011
Observations of wave propagation in landfast ice were obtained in Tempelfjorden, Svalbard during Mar...
The measured flexural strengths of freshwater ice and sea ice have been compiled with a view towards...
The vertical deflection of floating ice sheets subjected to the movements of an underwater object is...
Wave-ice interactions involve complex physical processes. Well-designed laboratory investigations ar...
An experiment on the propagation of flexural-gravity waves was performed in the HSVA ice tank in 201...
Air-coupled flexural waves (ACFWs) appear as wave trains of constant frequency that arrive in advanc...
Waves and swell incident on a continuous cover of sea ice can become coupled to the ice and propagat...
An experimental investigation of flexural-gravity waves was performed in the Hamburg Ship Model Basi...
There are many methods of determining elasticity that can be used on ice. These can be divided into...
The flexural strength of sea ice in situ was measured by a cantilever method. The measurement was ca...
The effective elastic modulus of ice is an important physical parameter for the calculation of ice s...
Two methods were used to locate the grounding line on the Rutford Ice Stream. The first method deter...
The flexural-gravity symmetric waves propagating in an ice channel with a lead of open water in the ...
This dataset includes the results of flexural and compression tests of sea ice samples conducted in ...
Geophysical surveying of the Arctic will become increasingly important in future prospecting and mon...
Observations of wave propagation in landfast ice were obtained in Tempelfjorden, Svalbard during Mar...
The measured flexural strengths of freshwater ice and sea ice have been compiled with a view towards...
The vertical deflection of floating ice sheets subjected to the movements of an underwater object is...
Wave-ice interactions involve complex physical processes. Well-designed laboratory investigations ar...
An experiment on the propagation of flexural-gravity waves was performed in the HSVA ice tank in 201...
Air-coupled flexural waves (ACFWs) appear as wave trains of constant frequency that arrive in advanc...
Waves and swell incident on a continuous cover of sea ice can become coupled to the ice and propagat...
An experimental investigation of flexural-gravity waves was performed in the Hamburg Ship Model Basi...
There are many methods of determining elasticity that can be used on ice. These can be divided into...
The flexural strength of sea ice in situ was measured by a cantilever method. The measurement was ca...
The effective elastic modulus of ice is an important physical parameter for the calculation of ice s...
Two methods were used to locate the grounding line on the Rutford Ice Stream. The first method deter...
The flexural-gravity symmetric waves propagating in an ice channel with a lead of open water in the ...
This dataset includes the results of flexural and compression tests of sea ice samples conducted in ...
Geophysical surveying of the Arctic will become increasingly important in future prospecting and mon...
Observations of wave propagation in landfast ice were obtained in Tempelfjorden, Svalbard during Mar...
The measured flexural strengths of freshwater ice and sea ice have been compiled with a view towards...
The vertical deflection of floating ice sheets subjected to the movements of an underwater object is...