Freshwater discharge from glaciers is increasing across the Arctic in response to
anthropogenic climate change, which raises questions about the potential downstream …

Four decades of studies on pristine Baffin Island fjords are summarized with respect to
sediment redistribution processes and resulting deposits. Sediment fill in these fjords …

Fjords are glacially carved estuaries that profoundly influence ice-sheet stability by draining
and ablating ice. Although abundant on modern high-latitude continental shelves, fjord …

The subantarctic islands between 40 and 60° S are circum-polar landmasses influenced by
the southern westerly wind (SWW) belt whose latitudinal shifts are driven by the Southern …

Iceberg discharge influences ocean circulation, affects climate and increases global sea
level. Icebergs are also known to gouge the seafloor in water depths limited by their keel …

Submarine channels are the primary conduits for terrestrial sediment, organic carbon, and
pollutant transport to the deep sea. Submarine channels are far more difficult to monitor than …

Recognition of Froude supercritical flow deposits in environments that range from rivers to
the ocean floor has triggered a surge of interest in their flow processes, bedforms and …

Quantification of the controls on turbidity current recurrence is required to better constrain
land to sea fluxes of sediment, carbon and pollutants, and design resilient infrastructure that …

Increased ocean heat supply to the Antarctic continental shelves is projected to cause
accelerated ice sheet loss and contribute significantly to global sea-level rise over coming …

Deep‐water deposits are important archives of Earth's history including the occurrence of
powerful flow events and the transfer of large volumes of terrestrial detritus into the world's …