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Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

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Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica. / Meredith, Michael; Inall, Mark; Brearley, Alexander et al.
Yn: Science Advances, Cyfrol 8, Rhif 47, eadd0720 , 25.11.2022, t. eadd0720.

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

HarvardHarvard

Meredith, M, Inall, M, Brearley, A, Ehmen, T, Sheen, K, Munday, D, Cook, A, Retallick, K, Van Landeghem, K, Gerrish, L, Annett, A, Carvalho, F, Jones, R, Naveira-Garabato, AC, Bull, C, Wallis, B, Hogg, A & Scourse, J 2022, 'Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica', Science Advances, cyfrol. 8, rhif 47, eadd0720 , tt. eadd0720. https://doi.org/10.1126/sciadv.add0720

APA

Meredith, M., Inall, M., Brearley, A., Ehmen, T., Sheen, K., Munday, D., Cook, A., Retallick, K., Van Landeghem, K., Gerrish, L., Annett, A., Carvalho, F., Jones, R., Naveira-Garabato, A. C., Bull, C., Wallis, B., Hogg, A., & Scourse, J. (2022). Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica. Science Advances, 8(47), eadd0720. Erthygl eadd0720 . https://doi.org/10.1126/sciadv.add0720

CBE

Meredith M, Inall M, Brearley A, Ehmen T, Sheen K, Munday D, Cook A, Retallick K, Van Landeghem K, Gerrish L, et al. 2022. Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica. Science Advances. 8(47):eadd0720. https://doi.org/10.1126/sciadv.add0720

MLA

Meredith, Michael et al. "Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica". Science Advances. 2022, 8(47). eadd0720. https://doi.org/10.1126/sciadv.add0720

VancouverVancouver

Meredith M, Inall M, Brearley A, Ehmen T, Sheen K, Munday D et al. Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica. Science Advances. 2022 Tach 25;8(47):eadd0720. eadd0720 . doi: 10.1126/sciadv.add0720

Author

Meredith, Michael ; Inall, Mark ; Brearley, Alexander et al. / Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica. Yn: Science Advances. 2022 ; Cyfrol 8, Rhif 47. tt. eadd0720.

RIS

TY - JOUR

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

AU - Meredith, Michael

AU - Inall, Mark

AU - Brearley, Alexander

AU - Ehmen, Tobias

AU - Sheen, Katy

AU - Munday, David

AU - Cook, Alison

AU - Retallick, Kate

AU - Van Landeghem, Katrien

AU - Gerrish, Laura

AU - Annett, Amber

AU - Carvalho, Filipa

AU - Jones, Rhiannon

AU - Naveira-Garabato, Alberto C.

AU - Bull, Christopher

AU - Wallis, Benjamin

AU - Hogg, Anna

AU - Scourse, James

PY - 2022/11/25

Y1 - 2022/11/25

N2 - Ocean mixing around Antarctica exerts key influences on glacier dynamics and ice shelf retreats, sea ice, and marine productivity, thus affecting global sea level and climate. The conventional paradigm is that this is dominated by winds, tides, and buoyancy forcing. Direct observations from the Antarctic Peninsula demonstrate that glacier calving triggers internal tsunamis, the breaking of which drives vigorous mixing. Being widespread and frequent, these internal tsunamis are at least comparable to winds, and much more important than tides, in driving regional shelf mixing. They are likely relevant everywhere that marine-terminating glaciers calve, including Greenland and across the Arctic. Calving frequency may change with higher ocean temperatures, suggesting possible shifts to internal tsunamigenesis and mixing in a warming climate.

AB - Ocean mixing around Antarctica exerts key influences on glacier dynamics and ice shelf retreats, sea ice, and marine productivity, thus affecting global sea level and climate. The conventional paradigm is that this is dominated by winds, tides, and buoyancy forcing. Direct observations from the Antarctic Peninsula demonstrate that glacier calving triggers internal tsunamis, the breaking of which drives vigorous mixing. Being widespread and frequent, these internal tsunamis are at least comparable to winds, and much more important than tides, in driving regional shelf mixing. They are likely relevant everywhere that marine-terminating glaciers calve, including Greenland and across the Arctic. Calving frequency may change with higher ocean temperatures, suggesting possible shifts to internal tsunamigenesis and mixing in a warming climate.

U2 - 10.1126/sciadv.add0720

DO - 10.1126/sciadv.add0720

M3 - Article

C2 - 36417533

VL - 8

SP - eadd0720

JO - Science Advances

JF - Science Advances

SN - 2375-2548

IS - 47

M1 - eadd0720

ER -