Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ...

AbstractWarmer and more persistent intrusions of Circumpolar Deep Water (CDW) onto the West Antarctic Peninsula are a key driver of the recent increase in ice shelf mass loss. The relatively warm and salty CDW is thought to be mixed up to the base of the ice shelves via shear‐driven turbulence where...

Full description

Bibliographic Details
Main Authors: Middleton, L, Davis, PED, Taylor, Nicholls, KW
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union (AGU) 2022
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.82111
https://www.repository.cam.ac.uk/handle/1810/334693
id ftdatacite:10.17863/cam.82111
record_format openpolar
spelling ftdatacite:10.17863/cam.82111 2024-02-27T08:33:15+00:00 Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ... Middleton, L Davis, PED Taylor, Nicholls, KW 2022 https://dx.doi.org/10.17863/cam.82111 https://www.repository.cam.ac.uk/handle/1810/334693 en eng American Geophysical Union (AGU) turbulence ice shelf boundary layer double diffusion article-journal ScholarlyArticle JournalArticle Article 2022 ftdatacite https://doi.org/10.17863/cam.82111 2024-02-01T15:03:26Z AbstractWarmer and more persistent intrusions of Circumpolar Deep Water (CDW) onto the West Antarctic Peninsula are a key driver of the recent increase in ice shelf mass loss. The relatively warm and salty CDW is thought to be mixed up to the base of the ice shelves via shear‐driven turbulence where it has a high capacity to melt the ice. We analyze data from a year‐long mooring beneath George VI Ice Shelf at a location where double‐diffusive layering was observed. The turbulent dissipation rates do not vary with mean flow speed, suggesting shear‐driven mixing is not the driver of basal melt at this site. Instead, we predict the observed dissipation using a new method that links along‐isopycnal stirring of temperature anomalies with double‐diffusive convection. Our work suggests that along‐isopycnal temperature variance may be a stronger indicator of melt than flow speed within strongly stratified ice shelf‐ocean boundary layers. ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula George VI Ice Shelf Ice Shelf Ice Shelves DataCite Metadata Store (German National Library of Science and Technology) Antarctic Antarctic Peninsula George VI Ice Shelf ENVELOPE(-67.840,-67.840,-71.692,-71.692)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic turbulence
ice shelf
boundary layer
double diffusion
spellingShingle turbulence
ice shelf
boundary layer
double diffusion
Middleton, L
Davis, PED
Taylor,
Nicholls, KW
Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ...
topic_facet turbulence
ice shelf
boundary layer
double diffusion
description AbstractWarmer and more persistent intrusions of Circumpolar Deep Water (CDW) onto the West Antarctic Peninsula are a key driver of the recent increase in ice shelf mass loss. The relatively warm and salty CDW is thought to be mixed up to the base of the ice shelves via shear‐driven turbulence where it has a high capacity to melt the ice. We analyze data from a year‐long mooring beneath George VI Ice Shelf at a location where double‐diffusive layering was observed. The turbulent dissipation rates do not vary with mean flow speed, suggesting shear‐driven mixing is not the driver of basal melt at this site. Instead, we predict the observed dissipation using a new method that links along‐isopycnal stirring of temperature anomalies with double‐diffusive convection. Our work suggests that along‐isopycnal temperature variance may be a stronger indicator of melt than flow speed within strongly stratified ice shelf‐ocean boundary layers. ...
format Article in Journal/Newspaper
author Middleton, L
Davis, PED
Taylor,
Nicholls, KW
author_facet Middleton, L
Davis, PED
Taylor,
Nicholls, KW
author_sort Middleton, L
title Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ...
title_short Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ...
title_full Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ...
title_fullStr Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ...
title_full_unstemmed Double Diffusion As a Driver of Turbulence in the Stratified Boundary Layer Beneath George VI Ice Shelf ...
title_sort double diffusion as a driver of turbulence in the stratified boundary layer beneath george vi ice shelf ...
publisher American Geophysical Union (AGU)
publishDate 2022
url https://dx.doi.org/10.17863/cam.82111
https://www.repository.cam.ac.uk/handle/1810/334693
long_lat ENVELOPE(-67.840,-67.840,-71.692,-71.692)
geographic Antarctic
Antarctic Peninsula
George VI Ice Shelf
geographic_facet Antarctic
Antarctic Peninsula
George VI Ice Shelf
genre Antarc*
Antarctic
Antarctic Peninsula
George VI Ice Shelf
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctic
Antarctic Peninsula
George VI Ice Shelf
Ice Shelf
Ice Shelves
op_doi https://doi.org/10.17863/cam.82111
_version_ 1792044786135334912