Simulation of the satellite radar altimeter sea ice thickness retrieval uncertainty

In the paper “A combined approach of remote sens- ing and airborne electromagnetics to determine the volume of polynya sea ice in the Laptev Sea” by L.. Rabenstein

One major di ff erence lies in the specific combination of bed deep- ness and ice thickness: while a large area of the ice sheet in the Weddell Sea Sector (namely the Institute

We were able to reproduce the results of the granular model using both the modified Coulombic yield curve of Hibler and Schulson (2000) and the elliptic yield curve of Hibler

In the present study, little auks foraged in the same areas in the presence and nearby absence of sea ice (Fig 1 and S1 Fig), thus questioning the importance of sea-ice habitats

The top 2 cm section of the sea ice had relative high bulk salinity on 20 January (Fig. 3) likely due to the granular nature of the sea ice in this part of the core creating

4, we finally compare the magnitude and pacing of past temperature changes reconstructed from deep ice cores to the changes simulated by coupled ocean-atmosphere-sea- ice models

The reconstructions are based on a multilinear regression of forecasted ice concentration, level ice thickness, ridge density, ice speed and an additional factor which is based,

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