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One source of information is numerical modelling of ice sheets.
The possibility of GIA causing the horizontal motions at SOHO and HVOL has been previously investigated based on modelling of ice mass loss over Katla alone.
Improved modelling of ice sheets, by use of high resolution and with representation of more physical processes, is constrained by long run-times even on the latest single-processor workstation.
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Models of ice dynamics should determine the most effective locations for pinning.
Jenkins, A. A one-dimensional model of ice shelf-ocean interaction.
A climate-dependent model of ice dynamics is employed to determine ice coverage and ice flux.
A mathematical model of ice formation in living cells during freezing is considered.
The researchers are now analyzing the data for future publication, to better understand how seawater interacts with the ice shelves and improve models of ice sheet behavior.
Traditionally, researchers run a model of ice flow and compare it to observations of the position and velocity of a glacier over time.
The measurements of temperature properties will help complete the puzzle of how the ocean and ice are interacting, leading researchers to build better models of ice sheet changes and sea-level rise.
We present a seven stage model of ice sheet evolution, from initiation to demise, in the form of palaeo-geographic maps.
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