Cross shelf-break exchange is limited by the tendency of geostrophic flow to follow
bathymetric contours, not cross them. However, small scale topography, such as canyons …

Poleward transport of warm Circumpolar Deep Water (CDW) has been linked to melting of
Antarctic ice shelves. However, even the steady-state spatial distribution and mechanisms of …

Predicting the source areas for Antarctic Bottom Water (AABW) requires knowledge of how
cold, dense water masses form and move from the Antarctic shelves to the continental slope …

The transport of oceanic heat towards the Antarctic continental margin is central to the mass
balance of the Antarctic Ice Sheet. Recent modeling efforts challenge our view on where and …

We report on observations of dense shelf water overflows and Antarctic Bottom Water
(AABW) formation along the continental margin of the Adélie and George V Land coast …

Submarine canyons are spectacular topographical features that intersect the continental
margins of the world's oceans. Canyons comprise unique habitats in terms of complexity …

The characteristics of Pacific‐born storms that cause upwelling along the Beaufort Sea
continental slope, the oceanographic response, and the modulation of the response due to …

The Totten Glacier is rapidly losing mass. It has been suggested that this mass loss is driven
by changes in oceanic forcing; however, the details of the ice–ocean interaction are …

We explore dense water cascading (DWC), a type of bottom‐trapped gravity current, on
multidecadal time scales using a pan‐Arctic regional ocean‐ice model. DWC is particularly …

Abstract Williams, A., Bax, NJ, Kloser, RJ, Althaus, F., Barker, B., and Keith G. 2009.
Australia's deep-water reserve network: implications of false homogeneity for classifying …