Inorganic carbon dynamics of melt-pond-covered first-year sea ice in the Canadian Arctic

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

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

number of strandings of migrants species results from the release of ice barriers and distribution changes in winter and early summer [51]; low ice volume into the Gulf could yield

The East Siberian Ice Sheet loses mass by surface melt along all margins except for the Arctic Ocean coast, where the losses occur by calving and shelf basal melt only.. Further

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 joint effect of fast increase of total energy consumption, rapid decline of Arctic sea ice extent and reduced precipitation and surface winds intensified the haze pollution

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

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