Recent research shows increasing decadal ice mass losses from the Greenland and
Antarctic Ice Sheets and more generally from glaciers worldwide in the light of continued …

Widespread existing geological records from above the modern ice-sheet surface and
outboard of the current ice margin show that the Antarctic Ice Sheet (AIS) was much more …

We compare the performance of five different regional climate models (RCMs)(COSMO-CLM
2, HIRHAM5, MAR3. 10, MetUM, and RACMO2. 3p2), forced by ERA-Interim reanalysis, in …

Climate trends in the Antarctic region remain poorly characterized, owing to the brevity and
scarcity of direct climate observations and the large magnitude of interannual to decadal …

Firn simulations are essential for understanding Antarctic ice sheet mass change, as they
enable us to convert satellite altimetry observed volume changes to mass changes and …

We present a 2700-year annually resolved chronology and snow accumulation history for
the Roosevelt Island Climate Evolution (RICE) ice core, Ross Ice Shelf, West Antarctica. The …

The isotopic signal (δ 18 O and δD) imprinted in ice cores from Antarctica is not solely
generated by the temperature sensitivity of the isotopic composition of precipitation but also …

Conversion of altimetry-derived ice-sheet volume change to mass requires an
understanding of the evolution of the combined ice and air content within the firn column. In …

The largest regional drivers of current surface elevation increases in the Antarctic Ice Sheet
are associated with ice flow reconfiguration in previously active ice streams, highlighting the …

High-resolution, well-dated climate archives provide an opportunity to investigate the
dynamic interactions of climate patterns relevant for future projections. Here, we present …