Joughin et al. (2010) applied
a numerical ice sheet model to predicting the future of PIG, their model suggested ongoing loss of ice mass from PIG, with a maximum rate of global sea level rise of 2.7 cm per century.
Indeed, many
numerical ice sheet models of Greenland assume that a uniform value of geothermal heat flux exists everywhere across Greenland.
The sea - level estimates are consistent with those from delta18O curves and
numerical ice sheet models, and imply a significant sensitivity of the WAIS and the coastal margins of the EAIS to orbital oscillations in insolation during the Mid-Pliocene period of relative global warmth.
An improved Antarctic dataset for high resolution
numerical ice sheet models (ALBMAP v1).
The researchers conclude: «Our findings imply that the outlet glaciers of Greenland, and the ice sheet as a whole, are probably more vulnerable to ocean thermal forcing and peripheral thinning than inferred previously from existing
numerical ice sheet models.»
Not exact matches
Constraints such as these are important for
numerical models that attempt to replicate and predict the past and future behaviour of the Antarctic
Ice Sheet.
A
numerical model of interactions between a marine
ice sheet and the solid earth: Application to a West Antarctic
ice stream.
A new
numerical model of coupled inland,
ice stream, and
ice shelf flow and its application to the West Antarctic
ice sheet, JGR.
This information is vital for
numerical models, and answers questions about how dynamic
ice sheets are, and how responsive they are to changes in atmospheric and oceanic temperatures.
The results are very conservative because they exclude the possibility of rapid changes of the
ice sheets as the
numerical models do not yet know how to deal with those.
They used the
Ice Sheet System Model (ISSM), a numerical depiction of the physics of ice sheets developed by scientists at JPL and the University of California, Irvi
Ice Sheet System
Model (ISSM), a
numerical depiction of the physics of
ice sheets developed by scientists at JPL and the University of California, Irvi
ice sheets developed by scientists at JPL and the University of California, Irvine.
JIGSAW (GEO) is a set of algorithms designed to generate complex, variable resolution unstructured meshes for geophysical
modelling applications, including: global ocean and atmospheric simulation,
numerical weather prediction, coastal ocean
modelling and
ice -
sheet dynamics.
This
ice sheet melted long time ago, but left behind geological evidence of sub glacial processes that now can be put in
numerical models, to test hypotheses of how they may work in modern environment.