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 …

Ice dynamic change is the primary cause of mass loss from the Antarctic Ice Sheet, thus it is
important to understand the processes driving ice-ocean interactions and the timescale on …

The Cook Glacier drains a significant portion of the Wilkes Subglacial Basin, the largest
subglacial basin in East Antarctica—which feeds the Cook Ice Shelf. The ice velocity of the …

We observe the evacuation of 11-year old land-fast sea ice in the Larsen-B Embayment on
the East Antarctic Peninsula in January 2022, which was in part triggered by warm …

Abstract The Greenland Ice Sheet is losing mass at increasing rates. Substantial amounts of
this mass loss occur by ice discharge which is influenced by ocean thermal forcing. The ice …

Land‐ice flow in Antarctica has experienced multi‐annual acceleration in response to
increased rates of ice thinning, ice‐shelf collapse and grounding‐line retreat. Superimposed …

Abstract The West Antarctic Ice Sheet is experiencing rapid thinning of its floating ice
shelves, largely attributed to oceanic basal melt. Numerical models suggest that the …

Few studies have assessed a comprehensive understanding of how the seasonal and
interannual variability and trends of the surface mass balance (SMB), including the influence …

The challenge of this century is without a doubt to counter global warming. Land
management, agriculture, and forests are responsible for 23% of total greenhouse gases …

Glaciers cover 132 900 km2 around the Antarctic Ice Sheet, but few are subject to annual
mass-balance measurements. Lookalike Glacier and Davies Dome on James Ross Island …