TY - CONF

T1 - Internal tsunamigenesis and mixing driven by glacier calving in Antarctica

AU - Meredith, Michael

AU - Inall, Mark

AU - Brearley, Alexander

AU - Munday, David

AU - Ehmen, Tobias

AU - Retallick, Kate

AU - Annett, Amber

AU - Jones, Rhiannon

AU - Carvalho, Filipa

AU - Van Landeghem, Katrien

AU - Garabato, Alberto Naveira

AU - Gerrish, Laura

AU - Scourse, James

AU - Cook, Alison

AU - Bull, Christopher

PY - 2022/5/23

Y1 - 2022/5/23

N2 - Ocean mixing around Antarctica is a key process that influences the vertical distributions of heat and nutrients, affecting glacier and ice shelf retreats, sea ice formation and marine productivity, with implications for regional ecosystems, global sea level and climate. Here we show that collapsing glacier fronts associated with calving events trigger internal tsunamis, the propagation and breaking of which can lead to significant mixing. Observations of one such event at the West Antarctic Peninsula, during which 3-20 megatonnes of ice were discharged to the ocean, reveal rapidly-elevated internal wave kinetic energy and upper-ocean shear, with strong homogenisation of the water column. Scaling arguments indicate that, at the West Antarctic Peninsula, just a few such events per summer would make this process comparable in magnitude to winds, and much more significant than tides, in driving shelf mixing. We postulate that this process is likely relevant to all regions with calving marine-terminating glaciers, including also Greenland and the Arctic. Glacier calving is expected to increase in a warming climate, likely strengthening internal tsunamigenesis and mixing in these regions in the coming decades.

AB - Ocean mixing around Antarctica is a key process that influences the vertical distributions of heat and nutrients, affecting glacier and ice shelf retreats, sea ice formation and marine productivity, with implications for regional ecosystems, global sea level and climate. Here we show that collapsing glacier fronts associated with calving events trigger internal tsunamis, the propagation and breaking of which can lead to significant mixing. Observations of one such event at the West Antarctic Peninsula, during which 3-20 megatonnes of ice were discharged to the ocean, reveal rapidly-elevated internal wave kinetic energy and upper-ocean shear, with strong homogenisation of the water column. Scaling arguments indicate that, at the West Antarctic Peninsula, just a few such events per summer would make this process comparable in magnitude to winds, and much more significant than tides, in driving shelf mixing. We postulate that this process is likely relevant to all regions with calving marine-terminating glaciers, including also Greenland and the Arctic. Glacier calving is expected to increase in a warming climate, likely strengthening internal tsunamigenesis and mixing in these regions in the coming decades.

U2 - https://doi.org/10.5194/egusphere-egu22-1163

DO - https://doi.org/10.5194/egusphere-egu22-1163

M3 - Paper

T2 - The EGU General Assembly 2022

Y2 - 23 May 2022 through 27 May 2022

ER -