Buoyancy fluxes and submarine melt rates at vertical ice‐ocean interfaces are commonly
parameterized using theories derived for unbounded free plumes. A Large Eddy Simulation …

The ocean supplies large quantities of thermal energy to tidewater glaciers, but the
mechanisms behind the heat delivery are not fully understood. To examine heat flux …

At marine‐terminating glaciers, both buoyant plumes and local currents energize turbulent
exchanges that control ice melt. Because of challenges in making centimeter‐scale …

In tidewater glacier fjords, subglacial discharge drives a significant mixing mechanism near
glacier fronts and drives a strong exchange flow. Numerous studies (Cowton et al., 2015 …

Glacial fjords often contain ice mélange, a frozen conglomeration of icebergs and sea ice,
which has been postulated to influence both glacier dynamics and fjord circulation through …

South Georgia is a heavily glaciated sub‐Antarctic island in the Southern Ocean.
Cumberland Bay is the largest fjord on the island, split into two arms, each with a large …

Abstract The Greenland Ice Sheet has undergone rapid mass loss over the last four
decades, primarily through solid and liquid discharge at marine‐terminating outlet glaciers …

The exchange of heat and freshwater between glaciers and the ocean is dictated by the
circulation in glacial fjords and ice shelf cavities. Therefore, our ability to estimate and …

Glacial fjord circulation determines the import of oceanic heat to the Greenland Ice Sheet
and the export of ice sheet meltwater to the ocean. However, limited observations and the …

Glacier retreat and mass loss in Northeast Greenland have profound implications for global
sea-level rise, making it crucial to understand the complex dynamics of glacier-ocean …