«
Improving ice sheet models means we need even finer resolution,» Gogineni said.
Not exact matches
Diagnostic
modelling can be used to
improve the understanding of the processes controlling the behaviour of a particular
ice stream, or to study the importance of one or more physical process in an
ice sheet in general.
SALSA will gather data from permanent GPS stations to better understand subglacial water flow's influence on the larger
ice sheet system and
improve subglacial lake
modeling through comparing our
model's estimates against geochemical data.
Improving digital elevation
models over
ice sheets using AVHRR - based photoclinometry.
Scientific knowledge input into process based
models has much
improved, reducing uncertainty of known science for some components of sea - level rise (e.g. steric changes), but when considering other components (e.g.
ice melt from
ice sheets, terrestrial water contribution) science is still emerging, and uncertainties remain high.
An
improved Antarctic dataset for high resolution numerical
ice sheet models (ALBMAP v1).
The US CLIVAR Greenland
Ice Sheet - Ocean Interactions Working Group was formed to foster and promote interaction between the diverse oceanographic, glaciological, atmospheric and climate communities, including modelers and field and data scientists within each community, interested in glacier / ocean interactions around Greenland, to advance understanding of the process and ultimately
improve its representation in climate
models.
Reducing these uncertainties by
improving models of the processes that cause
ice sheets to lose mass is, therefore, a critical goal of Earth Science research.
Despite higher temperature change projections in this assessment, the sea level projections are slightly lower, primarily due to the use of
improved models which give a smaller contribution from glaciers and
ice sheets.
«All this data is giving us much better insight into how sea
ice and the
ice sheets are changing, and this will help us understand the processes and
improve our
models and forecasts,» Meier said.
For their study, Hansen and his colleagues combined ancient paleo - climate data with new satellite readings and an
improved model of the climate system to demonstrate that
ice sheets can melt at a «non-linear» rate: rather than an incremental melting as Earth's poles inexorably warm,
ice sheets might melt at exponential rates, shedding dangerous amounts of mass in a matter of decades, not millennia.
Much process - based research coupling field work, remote sensing, and
modeling is required to advance assessment of the likelihood of a threshold - crossing leading to abrupt sea - level rise from the
ice sheets, as well as to
improve projections of moregradual sea - level rise that could lead to threshold - crossing events in other systems.