Insolation and gacial meltwater influence on sea‐ice and circulation variability in the Northeastern Labrador Sea during the last glacial period

This may be a consequence of the very high sea-ice di ff usivities (SID) that have been allowed in the ensemble leading to increased brine rejection and AABW production. + 0.83 in

To investigate the influence of snow depth, sea ice density, and area on sea ice thick- ness and volume estimates we use freeboard retrievals from ICESat, together with dif-

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

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

We use this mixed GDGT signal in the central Red Sea to estimate the exchange rate with the Gulf of Aden relative to modern conditions, based on a simple two end-member mixing

We have analysed observa- tions of the summer sea ice edge from the ship logbooks of explorers such as Robert Falcon Scott, Ernest Shackleton and their contemporaries during the