Antarctic landfast sea ice (fast ice) is stationary sea ice that is attached to the coast,
grounded icebergs, ice shelves, or other protrusions on the continental shelf. Fast ice forms …

The variability of the Antarctic and Greenland ice sheets occurs on various timescales and is
important for projections of sea level rise; however, there are substantial uncertainties …

Recent studies have highlighted the prevalence of microplastic (MP) pollution in the global
marine environment and these pollutants have been found to contaminate even remote …

The information system PANGAEA provides targeted support for research data management
as well as long-term data archiving and publication. PANGAEA is operated as an open …

Fin whales (Balaenoptera physalus quoyi) of the Southern Hemisphere were brought to
near extinction by twentieth century industrial whaling. For decades, they had all but …

Satellite-derived bathymetry (SDB) is the process of estimating water depth in shallow
coastal and inland waters using satellite imagery. Recent advances in technology and data …

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 …

We employ a time series of Sentinel‐1 differential radar interferometry data from 2018 to
detect the variability in grounding line position of the Fisher, Mellor, and Lambert glaciers …

Bathymetry critically influences the intrusion of warm Circumpolar Deep Water onto the
continental shelf and under ice shelf cavities in Antarctica, thereby forcing ice melting …

The intrusion of relatively warm water onto the continental shelf is widely recognized as a
threat to Antarctic ice shelves and glaciers grounded below sea level, as enhanced ocean …