There is increasing evidence that fossil-fuel burning, and consequential global heating of
1.1° C to date, has led to the increased occurrence and severity of extreme environmental …

The largest uncertainty in future sea-level rise is loss of ice from the Greenland and Antarctic
Ice Sheets. Ice shelves, freely floating platforms of ice that fringe the ice sheets, play a …

Atmospheric rivers (ARs) that reach the Antarctic Ice Sheet (AIS) transport anomalous
moisture from lower latitudes and can impact the AIS via extreme precipitation and …

In late March 2011, landfast sea ice (hereafter,'fast ice') formed in the northern Larsen B
embayment and persisted continuously as multi-year fast ice until January 2022. In the 11 …

Antarctica is considered as an important component of the global climate system, not only
because of its ability to drive global sea-level rise through ice melting [1], but also because …

Calving glaciers respond quickly to atmospheric variability through ice dynamic adjustment.
Particularly, single weather extremes may cause changes in ice-flow velocity and terminus …

Polynyas, or ice-free regions within the sea ice pack, are a common occurrence around
Antarctica. A recurrent and often large polynya is the Terra Nova Bay Polynya (TNBP) …

Although rare, atmospheric rivers substantially influence the interannual variability of
Antarctic surface mass balance. Here we use MERRA-2 reanalysis to identify characteristics …

The mesoscale dynamics of a record‐breaking Atmospheric River (AR) that impacted the
Middle East in mid‐April 2023 and caused property damage and loss of life are investigated …

Pine Island Glacier (PIG) has recently experienced increased ice loss mostly attributed to
basal melt and ocean-ice dynamics. However, atmospheric forcing also plays a role in the …