The present-day state and future of the Antarctic Ice Sheet depend on the rate at which the
ocean melts its fringing ice shelves. Ocean heat must cross many physical and dynamical …

Feedbacks between ice melt, glacier flow and ocean circulation can rapidly accelerate ice
loss at tidewater glaciers and alter projections of sea-level rise. At the core of these …

Marine‐terminating glacier fjords play a central role in the transport of oceanic heat toward
ice sheets, regulating their melt. Mixing processes near glacial termini are key to this …

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

High-resolution spaceborne synthetic aperture radar (SAR) images have verified the wide
existence of internal solitary waves (ISWs) over the Chukchi and Beaufort Seas. A major ISW …

Marine-terminating glaciers are pathways for terrestrial ice to reach Arctic waters, thereby
contributing to sea level rise and changing global circulation patterns. One mechanism for …