The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing
In situ measurements of flow and stratification in the vicinity of the Erebus Glacier Tongue, a12 km long floating Antarctic glacier, show the significant influence of the glacier. Three ADCPs (75, 300,and 600 kHz) were deployed close (<50 m) to the sidewall of the glacier in order to capture nea...
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Online Access: | https://doi.org/10.1002/2013JC009070 http://ecite.utas.edu.au/91376 |
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ftunivtasecite:oai:ecite.utas.edu.au:91376 2023-05-15T13:42:40+02:00 The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing Stevens, CL McPhee, MG Forrest, AL Leonard, GH Stanton, T Haskell, TG 2014 application/pdf https://doi.org/10.1002/2013JC009070 http://ecite.utas.edu.au/91376 en eng Wiley-Blackwell Publishing, Inc. http://ecite.utas.edu.au/91376/1/91376_RODA_001.pdf http://dx.doi.org/10.1002/2013JC009070 Stevens, CL and McPhee, MG and Forrest, AL and Leonard, GH and Stanton, T and Haskell, TG, The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing, Journal of Geophysical Research: Oceans, 119, (4) pp. 2344-2362. ISSN 2169-9291 (2014) [Refereed Article] http://ecite.utas.edu.au/91376 Earth Sciences Oceanography Physical oceanography Refereed Article PeerReviewed 2014 ftunivtasecite https://doi.org/10.1002/2013JC009070 2022-09-05T22:16:46Z In situ measurements of flow and stratification in the vicinity of the Erebus Glacier Tongue, a12 km long floating Antarctic glacier, show the significant influence of the glacier. Three ADCPs (75, 300,and 600 kHz) were deployed close (<50 m) to the sidewall of the glacier in order to capture near-field flowdistortion. Scalar (temperature and conductivity) and shear microstructure profiling captured small-scalevertical variability. Flow magnitudes exceeded 0.3 m s21 through a combination of tidal flow (~8 cm s -1 )and a background/residual flow (~4-10 cm s -1 ) flowing to the NW. Turbulence was dominated by deepermixing during spring tide, likely indicative of the role of bathymetric variation which locally forms an obstacleas great as the glacier. During the neap tide, near-surface mixing was as energetic as that seen in thespring tide, suggesting the presence of buoyancy-driven near-surface flows. Estimates of integrated dissipationrate suggest that these floating extensions of the Antarctic ice sheet alter energy budgets throughenhanced dissipation, and thus influence coastal near-surface circulation. Article in Journal/Newspaper Antarc* Antarctic Erebus Glacier Ice Sheet eCite UTAS (University of Tasmania) Antarctic Erebus Glacier ENVELOPE(167.000,167.000,-77.683,-77.683) Erebus Glacier Tongue ENVELOPE(166.667,166.667,-77.700,-77.700) The Antarctic Journal of Geophysical Research: Oceans 119 4 2344 2362 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Physical oceanography |
spellingShingle |
Earth Sciences Oceanography Physical oceanography Stevens, CL McPhee, MG Forrest, AL Leonard, GH Stanton, T Haskell, TG The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing |
topic_facet |
Earth Sciences Oceanography Physical oceanography |
description |
In situ measurements of flow and stratification in the vicinity of the Erebus Glacier Tongue, a12 km long floating Antarctic glacier, show the significant influence of the glacier. Three ADCPs (75, 300,and 600 kHz) were deployed close (<50 m) to the sidewall of the glacier in order to capture near-field flowdistortion. Scalar (temperature and conductivity) and shear microstructure profiling captured small-scalevertical variability. Flow magnitudes exceeded 0.3 m s21 through a combination of tidal flow (~8 cm s -1 )and a background/residual flow (~4-10 cm s -1 ) flowing to the NW. Turbulence was dominated by deepermixing during spring tide, likely indicative of the role of bathymetric variation which locally forms an obstacleas great as the glacier. During the neap tide, near-surface mixing was as energetic as that seen in thespring tide, suggesting the presence of buoyancy-driven near-surface flows. Estimates of integrated dissipationrate suggest that these floating extensions of the Antarctic ice sheet alter energy budgets throughenhanced dissipation, and thus influence coastal near-surface circulation. |
format |
Article in Journal/Newspaper |
author |
Stevens, CL McPhee, MG Forrest, AL Leonard, GH Stanton, T Haskell, TG |
author_facet |
Stevens, CL McPhee, MG Forrest, AL Leonard, GH Stanton, T Haskell, TG |
author_sort |
Stevens, CL |
title |
The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing |
title_short |
The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing |
title_full |
The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing |
title_fullStr |
The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing |
title_full_unstemmed |
The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing |
title_sort |
influence of an antarctic glacier tongue on near-field ocean circulation and mixing |
publisher |
Wiley-Blackwell Publishing, Inc. |
publishDate |
2014 |
url |
https://doi.org/10.1002/2013JC009070 http://ecite.utas.edu.au/91376 |
long_lat |
ENVELOPE(167.000,167.000,-77.683,-77.683) ENVELOPE(166.667,166.667,-77.700,-77.700) |
geographic |
Antarctic Erebus Glacier Erebus Glacier Tongue The Antarctic |
geographic_facet |
Antarctic Erebus Glacier Erebus Glacier Tongue The Antarctic |
genre |
Antarc* Antarctic Erebus Glacier Ice Sheet |
genre_facet |
Antarc* Antarctic Erebus Glacier Ice Sheet |
op_relation |
http://ecite.utas.edu.au/91376/1/91376_RODA_001.pdf http://dx.doi.org/10.1002/2013JC009070 Stevens, CL and McPhee, MG and Forrest, AL and Leonard, GH and Stanton, T and Haskell, TG, The influence of an Antarctic glacier tongue on near-field ocean circulation and mixing, Journal of Geophysical Research: Oceans, 119, (4) pp. 2344-2362. ISSN 2169-9291 (2014) [Refereed Article] http://ecite.utas.edu.au/91376 |
op_doi |
https://doi.org/10.1002/2013JC009070 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
119 |
container_issue |
4 |
container_start_page |
2344 |
op_container_end_page |
2362 |
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1766171339807260672 |