The Greenland Ice Mapping Project (GIMP) land classification and surface elevation data sets

We apply a new parameterisation of the Greenland ice sheet (GrIS) feedback between surface mass balance (SMB: the sum of surface accumulation and surface ablation) and surface

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 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

The CPR products considered here are the vertical profiles of cloud ice water content (IWC) and the effective radius (ER) of ice particles, which are compared with the number of

The averaged MODIS ice thickness in 12.5 km grid resolution (upper left), SMOS ice thicknesses retrieved from Algorithm I (upper right) and II (lower left), and the histogram of

The SMB anomaly projection for k = a/b =− 1 as well as the cumulated sea level rises equivalent are shown in Fig. This record surface mass loss rate is likely to become com- mon at

P., Traversi, R., and Udisti, R.: Holocene volcanic history as recorded in the sulphate stratigraphy of the European Project for Ice Coring in Antarctica Dome C (EDC96) ice core, J.

When we try different values for the ice temperature, snow density, and ice salinity (not shown here), we find that only the ice salinity impacts the modelled brightness