Antarctic sea ice projections are

In this quantitative study of hydrous calcium carbonate as ikaite, sea ice cores and brine samples were collected from pack and land fast sea ice between September and December

Piot and von Glasow [2008] showed that the precipitation of calcium carbonate (CaCO 3 ) in sea ice brine is a key process allowing for the rapid acidi fi cation of aerosols

and colleagues conclude that, over the course of the twenty-first century, warm pulses of ocean currents are likely to reach this ice shelf and induce basal melt, whereas Ross

In order to investigate the role and the spatial and temporal variability of platelet ice and snow for Antarctic fast ice, we perform regular field measurements on the land-fast sea

and that which is produced by biological activity within the sea ice, the effect of physical concentration during brine formation through seawater freezing was removed using

Figure 5: Synchrotron X-ray diffraction patterns (lattice spacing d vs. diffracted intensity) of (a) crystals isolated from a sea ice core in the home laboratory, (b) crystals

The determination of the geochemical composition of sea ice brine is based on mea- surements of pH , total alkalinity, and calculations using different sets of dissociation

Sea level pressure means from NCEP Reanalysis data and ice concentration data from SSM/I give no evidence for the unusual drift pattern derived from satellite data for the first