The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and multi-site dating approach for the last 120 thousand years

The total elevation bias (black line) has a component due to horizon- tal advection (red line, given as the elevation difference between Kohnen and the place of origin of the

The aim of this study was to investigate the rate and patterns of colonization by terrestrial mites on ice-free areas created by the melting of maritime Antarctic glaciers..

The probability of attending school four our group of interest in this region increased by 6.5 percentage points after the expansion of the Bolsa Família program in 2007 and

of significant convective influence, the thermal signal in the shallow firn, the expected gravitational enrichment in the di ff usive column, the depth of the firn-ice transition,

These measurements contain in- formation on trace gases below the instrument and inside the snowpack, whereas the upward looking viewing directions are mainly sensitive for absorbers

Raw data gener- ated by the model are processed to obtain the time series of concentration and isotopic composition of atmospheric ni- trate and in a top skin layer of 4 mm, the

The low dating error and comparison with the NGRIP (North Greenland Ice Core Project) volcanic records (on the GICC05 timescale) suggest Law Dome is the most accurately dated

During the LGM and the last glacial transition while the East Antarctic Ice Sheet ad- vanced to the shelf break, coastal polynyas were active above the continental slope, which