Krill transport in the Scotia Sea and environs

Historical observations of the large-scale flow and frontal structure of the Antarctic Circumpolar Current in the Scotia Sea region were combined with the wind-induced surface Ekman transport to produce a composite flow field. This was used with a Lagrangian model to investigate transport of Antarct...

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Published in:Antarctic Science
Main Authors: Hofmann, Eileen E., Klinck, John M., Locarnini, Ricardo A., Fach, Bettina, Murphy, Eugene
Format: Article in Journal/Newspaper
Language:unknown
Published: Cambridge University Press 1998
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/504062/
https://doi.org/10.1017/S0954102098000492
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spelling ftnerc:oai:nora.nerc.ac.uk:504062 2023-05-15T13:48:08+02:00 Krill transport in the Scotia Sea and environs Hofmann, Eileen E. Klinck, John M. Locarnini, Ricardo A. Fach, Bettina Murphy, Eugene 1998 http://nora.nerc.ac.uk/id/eprint/504062/ https://doi.org/10.1017/S0954102098000492 unknown Cambridge University Press Hofmann, Eileen E.; Klinck, John M.; Locarnini, Ricardo A.; Fach, Bettina; Murphy, Eugene orcid:0000-0002-7369-9196 . 1998 Krill transport in the Scotia Sea and environs. Antarctic Science, 10 (04). 406-415. https://doi.org/10.1017/S0954102098000492 <https://doi.org/10.1017/S0954102098000492> Publication - Article PeerReviewed 1998 ftnerc https://doi.org/10.1017/S0954102098000492 2023-02-04T19:38:15Z Historical observations of the large-scale flow and frontal structure of the Antarctic Circumpolar Current in the Scotia Sea region were combined with the wind-induced surface Ekman transport to produce a composite flow field. This was used with a Lagrangian model to investigate transport of Antarctic krill. Particle displacements from known krill spawning areas that result from surface Ekman drift, a composite large-scale flow, and the combination of the two were calculated. Surface Ekman drift alone only transports particles a few kilometres over the 150-day krill larval development time. The large-scale composite flow moves particles several hundreds of kilometres over the same time, suggesting this is the primary transport mechanism. An important contribution of the surface Ekman drift on particles released along the continental shelf break west of the Antarctic Peninsula is moving them north-northeast into the high-speed core of the southern Antarctic Circumpolar Current Front, which then transports the particles to South Georgia in about 140–160 days. Similar particle displacement calculations using surface flow fields obtained from the Fine Resolution Antarctic Model do not show overall transport from the Antarctic Peninsula to South Georgia due to the inaccurate position of the southern Antarctic Circumpolar Current Front in the simulated circulation fields. The particle transit times obtained with the composite large-scale flow field are consistent with regional abundances of larval krill developmental stages collected in the Scotia Sea. These results strongly suggest that krill populations west of the Antarctic Peninsula provide the source for the krill populations found around South Georgia. Article in Journal/Newspaper Antarc* Antarctic Antarctic Krill Antarctic Peninsula Antarctic Science Scotia Sea Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula Scotia Sea Antarctic Science 10 4 406 415
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description Historical observations of the large-scale flow and frontal structure of the Antarctic Circumpolar Current in the Scotia Sea region were combined with the wind-induced surface Ekman transport to produce a composite flow field. This was used with a Lagrangian model to investigate transport of Antarctic krill. Particle displacements from known krill spawning areas that result from surface Ekman drift, a composite large-scale flow, and the combination of the two were calculated. Surface Ekman drift alone only transports particles a few kilometres over the 150-day krill larval development time. The large-scale composite flow moves particles several hundreds of kilometres over the same time, suggesting this is the primary transport mechanism. An important contribution of the surface Ekman drift on particles released along the continental shelf break west of the Antarctic Peninsula is moving them north-northeast into the high-speed core of the southern Antarctic Circumpolar Current Front, which then transports the particles to South Georgia in about 140–160 days. Similar particle displacement calculations using surface flow fields obtained from the Fine Resolution Antarctic Model do not show overall transport from the Antarctic Peninsula to South Georgia due to the inaccurate position of the southern Antarctic Circumpolar Current Front in the simulated circulation fields. The particle transit times obtained with the composite large-scale flow field are consistent with regional abundances of larval krill developmental stages collected in the Scotia Sea. These results strongly suggest that krill populations west of the Antarctic Peninsula provide the source for the krill populations found around South Georgia.
format Article in Journal/Newspaper
author Hofmann, Eileen E.
Klinck, John M.
Locarnini, Ricardo A.
Fach, Bettina
Murphy, Eugene
spellingShingle Hofmann, Eileen E.
Klinck, John M.
Locarnini, Ricardo A.
Fach, Bettina
Murphy, Eugene
Krill transport in the Scotia Sea and environs
author_facet Hofmann, Eileen E.
Klinck, John M.
Locarnini, Ricardo A.
Fach, Bettina
Murphy, Eugene
author_sort Hofmann, Eileen E.
title Krill transport in the Scotia Sea and environs
title_short Krill transport in the Scotia Sea and environs
title_full Krill transport in the Scotia Sea and environs
title_fullStr Krill transport in the Scotia Sea and environs
title_full_unstemmed Krill transport in the Scotia Sea and environs
title_sort krill transport in the scotia sea and environs
publisher Cambridge University Press
publishDate 1998
url http://nora.nerc.ac.uk/id/eprint/504062/
https://doi.org/10.1017/S0954102098000492
geographic Antarctic
The Antarctic
Antarctic Peninsula
Scotia Sea
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
Scotia Sea
genre Antarc*
Antarctic
Antarctic Krill
Antarctic Peninsula
Antarctic Science
Scotia Sea
genre_facet Antarc*
Antarctic
Antarctic Krill
Antarctic Peninsula
Antarctic Science
Scotia Sea
op_relation Hofmann, Eileen E.; Klinck, John M.; Locarnini, Ricardo A.; Fach, Bettina; Murphy, Eugene orcid:0000-0002-7369-9196 . 1998 Krill transport in the Scotia Sea and environs. Antarctic Science, 10 (04). 406-415. https://doi.org/10.1017/S0954102098000492 <https://doi.org/10.1017/S0954102098000492>
op_doi https://doi.org/10.1017/S0954102098000492
container_title Antarctic Science
container_volume 10
container_issue 4
container_start_page 406
op_container_end_page 415
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