Capabilities and performance of Elmer/Ice, a new-generation ice sheet model

Vertical thinning due to ice flow has been estimated both for the EDC and Dome Fuji ice cores based on a 1-D ice flow model (Parrenin et al., 2007b) with prescribed ice

The mean values and uncertainties of snow depth and ice and snow densities, determined for FY ice and MY ice, were used to calculate the total error in ice thickness retrieval

Boundary condi- tions such as sea surface temperatures (SSTs), topography, ice-sheet extent and vegetation are derived from the ones imposed by the Pliocene Model

and Marsiat, I.: Simulations of the Northern Hemisphere through the last glacial- interglacial cycle with a vertically integrated and a three-dimensional thermomechanical ice-

Unstructured finite element mesh and model surface velocities after optimisation of the basal friction with the Robin inverse method, on the whole ice sheet and zooms on

The idea of the proposed ice flow estimation method is based on parallax decomposition of two adjacent matched ice-flow features from two images acquired at different

In this article, we examine the consequence of submarine frontal melting and the ice mélange on glacier dynamics and on the behavior of the glacier front using a full- Stokes

We have described and demonstrated a new procedure for generating 1850 preindus- trial ice sheet states for use in fully coupled ice-sheet/climate models which results in