Winter-time oceanography of the Adelie Depression
The formation of high-salinity shelf waters beneath coastal polynyas from enhanced sea-ice production and brine rejection during wintertime is critical to the production of Antarctic Bottom Waters. We report on the first wintertime measurements of high-salinity shelf water formation over the Adlie D...
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ftunivtasecite:oai:ecite.utas.edu.au:34696 2023-05-15T14:03:55+02:00 Winter-time oceanography of the Adelie Depression Williams, GD Bindoff, NL 2003 https://doi.org/10.1016/S0967-0645(03)00074-2 http://ecite.utas.edu.au/34696 en eng Pergamon-Elsevier Science Ltd http://dx.doi.org/10.1016/S0967-0645(03)00074-2 Williams, GD and Bindoff, NL, Winter-time oceanography of the Adelie Depression, Deep-Sea Research ll, 50, (8-9) pp. 1373-1392. ISSN 0967-0645 (2003) [Refereed Article] http://ecite.utas.edu.au/34696 Earth Sciences Oceanography Physical Oceanography Refereed Article PeerReviewed 2003 ftunivtasecite https://doi.org/10.1016/S0967-0645(03)00074-2 2019-12-13T21:13:22Z The formation of high-salinity shelf waters beneath coastal polynyas from enhanced sea-ice production and brine rejection during wintertime is critical to the production of Antarctic Bottom Waters. We report on the first wintertime measurements of high-salinity shelf water formation over the Adlie Depression off the East Antarctic coast between 143 and 146E, during the Mertz Glacier Polynya Experiment in July-August 1999. The general circulation and evolution of water masses in the Adlie Depression during winter are described, and in particular we quantify the rates of brine rejection (sea-ice growth), ocean heat flux, and latent heat flux, in the Mertz polynya central to the formation of high-salinity shelf waters. We find shelf waters above the minimum sill depth with sufficient density to become Adlie Land Bottom Water and suggest the highest production rates occur near Commonwealth Bay. Sea-ice growth and heat transfer rates are calculated from the divergence of heat and freshwater fields around a closed volume beneath the Mertz polynya. The sea-ice growth estimates and associated Monte Carlo errors are found to range from 4.81.7, 4.11.5, 8.41.7 cm d-1, respectively, over a 3-week period. The average growth rate is 5.8 cm d-1. Near the Mertz polynya the sensible heat from ocean transport is between 15 6 and 43 11 W m-2, with an average of 30 W m-2, and the latent heat budget is between 125 45 and 254 52 W m-2, with an average of 174 W m-2. We conclude that during winter the Mertz polynya is primarily a latent heat polynya. Crown Copyright 2003 Published by Elsevier Science Ltd. All rights reserved. Article in Journal/Newspaper Antarc* Antarctic Mertz Glacier Sea ice eCite UTAS (University of Tasmania) Adelie Depression ENVELOPE(146.000,146.000,-67.417,-67.417) Antarctic Commonwealth Bay ENVELOPE(142.500,142.500,-67.000,-67.000) Mertz Glacier ENVELOPE(144.500,144.500,-67.667,-67.667) Deep Sea Research Part II: Topical Studies in Oceanography 50 8-9 1373 1392 |
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Open Polar |
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eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Physical Oceanography |
spellingShingle |
Earth Sciences Oceanography Physical Oceanography Williams, GD Bindoff, NL Winter-time oceanography of the Adelie Depression |
topic_facet |
Earth Sciences Oceanography Physical Oceanography |
description |
The formation of high-salinity shelf waters beneath coastal polynyas from enhanced sea-ice production and brine rejection during wintertime is critical to the production of Antarctic Bottom Waters. We report on the first wintertime measurements of high-salinity shelf water formation over the Adlie Depression off the East Antarctic coast between 143 and 146E, during the Mertz Glacier Polynya Experiment in July-August 1999. The general circulation and evolution of water masses in the Adlie Depression during winter are described, and in particular we quantify the rates of brine rejection (sea-ice growth), ocean heat flux, and latent heat flux, in the Mertz polynya central to the formation of high-salinity shelf waters. We find shelf waters above the minimum sill depth with sufficient density to become Adlie Land Bottom Water and suggest the highest production rates occur near Commonwealth Bay. Sea-ice growth and heat transfer rates are calculated from the divergence of heat and freshwater fields around a closed volume beneath the Mertz polynya. The sea-ice growth estimates and associated Monte Carlo errors are found to range from 4.81.7, 4.11.5, 8.41.7 cm d-1, respectively, over a 3-week period. The average growth rate is 5.8 cm d-1. Near the Mertz polynya the sensible heat from ocean transport is between 15 6 and 43 11 W m-2, with an average of 30 W m-2, and the latent heat budget is between 125 45 and 254 52 W m-2, with an average of 174 W m-2. We conclude that during winter the Mertz polynya is primarily a latent heat polynya. Crown Copyright 2003 Published by Elsevier Science Ltd. All rights reserved. |
format |
Article in Journal/Newspaper |
author |
Williams, GD Bindoff, NL |
author_facet |
Williams, GD Bindoff, NL |
author_sort |
Williams, GD |
title |
Winter-time oceanography of the Adelie Depression |
title_short |
Winter-time oceanography of the Adelie Depression |
title_full |
Winter-time oceanography of the Adelie Depression |
title_fullStr |
Winter-time oceanography of the Adelie Depression |
title_full_unstemmed |
Winter-time oceanography of the Adelie Depression |
title_sort |
winter-time oceanography of the adelie depression |
publisher |
Pergamon-Elsevier Science Ltd |
publishDate |
2003 |
url |
https://doi.org/10.1016/S0967-0645(03)00074-2 http://ecite.utas.edu.au/34696 |
long_lat |
ENVELOPE(146.000,146.000,-67.417,-67.417) ENVELOPE(142.500,142.500,-67.000,-67.000) ENVELOPE(144.500,144.500,-67.667,-67.667) |
geographic |
Adelie Depression Antarctic Commonwealth Bay Mertz Glacier |
geographic_facet |
Adelie Depression Antarctic Commonwealth Bay Mertz Glacier |
genre |
Antarc* Antarctic Mertz Glacier Sea ice |
genre_facet |
Antarc* Antarctic Mertz Glacier Sea ice |
op_relation |
http://dx.doi.org/10.1016/S0967-0645(03)00074-2 Williams, GD and Bindoff, NL, Winter-time oceanography of the Adelie Depression, Deep-Sea Research ll, 50, (8-9) pp. 1373-1392. ISSN 0967-0645 (2003) [Refereed Article] http://ecite.utas.edu.au/34696 |
op_doi |
https://doi.org/10.1016/S0967-0645(03)00074-2 |
container_title |
Deep Sea Research Part II: Topical Studies in Oceanography |
container_volume |
50 |
container_issue |
8-9 |
container_start_page |
1373 |
op_container_end_page |
1392 |
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