Ocean mixing and heat transport processes observed under the Ross Ice Shelf control its basal melting.

Antarctic oceanography basal melting ice shelf cavity interleaving ocean mixing

Journal

Proceedings of the National Academy of Sciences of the United States of America
ISSN: 1091-6490
Titre abrégé: Proc Natl Acad Sci U S A
Pays: United States
ID NLM: 7505876

Informations de publication

Date de publication:
21 07 2020
Historique:
pubmed: 1 7 2020
medline: 1 7 2020
entrez: 1 7 2020
Statut: ppublish

Résumé

The stability of large Antarctic ice shelves has important implications for global sea level, sea ice area, and ocean circulation. A significant proportion of ice mass loss from these ice shelves is through ocean-driven melting which is controlled by largely unobserved oceanic thermodynamic and circulatory processes in the cavity beneath the ice shelf. Here we use direct measurements to provide evidence of the changing water column structure in the cavity beneath the Ross Ice Shelf, the planet's largest ice shelf by area. The cavity water column data exhibit both basal and benthic boundary layers, along with evidence of tidally modulated and diffusively convecting internal mixing processes. A region of thermohaline interleaving in the upper-middle water column indicates elevated diffusion and the potential to modify the cavity circulation. The measurements were recorded using the Aotearoa New Zealand Ross Ice Shelf Program hot water drill borehole melted in the central region of the shelf in December 2017 (HWD2), only the second borehole through the central region of the ice shelf, following J9 in 1977. These data, and comparison with the 1977 data, provide valuable insight into ice shelf cavity circulation and aid understanding of the evolution of the presently stable Ross Ice Shelf.

Identifiants

pubmed: 32601211
pii: 1910760117
doi: 10.1073/pnas.1910760117
pmc: PMC7382223
doi:

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

16799-16804

Informations de copyright

Copyright © 2020 the Author(s). Published by PNAS.

Déclaration de conflit d'intérêts

The authors declare no competing interest.

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Auteurs

Craig Stevens (C)

Ocean Dynamics Group, New Zealand National Institute of Water and Atmospheric Research, Wellington 6241, New Zealand; craig.stevens@niwa.co.nz.
Department of Physics, University of Auckland, Auckland 1010, New Zealand.

Christina Hulbe (C)

Department of Surveying, University of Otago, Dunedin 9016, New Zealand.

Mike Brewer (M)

Ocean Dynamics Group, New Zealand National Institute of Water and Atmospheric Research, Wellington 6241, New Zealand.

Craig Stewart (C)

Ocean Dynamics Group, New Zealand National Institute of Water and Atmospheric Research, Wellington 6241, New Zealand.

Natalie Robinson (N)

Ocean Dynamics Group, New Zealand National Institute of Water and Atmospheric Research, Wellington 6241, New Zealand.

Christian Ohneiser (C)

Department of Geology, University of Otago, Dunedin 9054, New Zealand.

Stefan Jendersie (S)

Antarctic Research Centre, Victoria University of Wellington, Wellington 6140, New Zealand.

Classifications MeSH