Nearshore mixing and nutrient delivery along the western Antarctic Peninsula
Abstract The surface waters of the Southern Ocean play a key role in the global climate and carbon cycles by promoting growth of some of the world’s largest phytoplankton blooms. Several studies have emphasized the importance of glacial and sediment inputs of Fe that fuel the primary production of t...
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Online Access: | http://dx.doi.org/10.1017/s095410201700013x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201700013X |
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crcambridgeupr:10.1017/s095410201700013x 2024-03-03T08:38:12+00:00 Nearshore mixing and nutrient delivery along the western Antarctic Peninsula Corbett, D. Reide Crenshaw, Jared Null, Kimberly Peterson, Richard N. Peterson, Leigha E. Lyons, W. Berry 2017 http://dx.doi.org/10.1017/s095410201700013x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201700013X en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Antarctic Science volume 29, issue 5, page 397-409 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2017 crcambridgeupr https://doi.org/10.1017/s095410201700013x 2024-02-08T08:24:59Z Abstract The surface waters of the Southern Ocean play a key role in the global climate and carbon cycles by promoting growth of some of the world’s largest phytoplankton blooms. Several studies have emphasized the importance of glacial and sediment inputs of Fe that fuel the primary production of the Fe-limited Southern Ocean. Although the fertile surface waters along the shelf of the western Antarctic Peninsula (WAP) are influenced by large inputs of freshwater, this freshwater may take multiple pathways (e.g. calving, streams, groundwater discharge) with different degrees of water-rock interactions leading to variable Fe flux to coastal waters. During the summers of 2012–13 and 2013–14, seawater samples were collected along the WAP, near Anvers Island, to observe water column dynamics in nearshore and offshore waters. Tracers ( 223,224 Ra, 222 Rn, 18 O, 2 H) were used to evaluate the source and transport of water and nutrients in coastal fjords and across the shelf. Coastal waters are compared across two field seasons, with increased freshwater observed during 2014. Horizontal mixing rates of water masses along the WAP ranged from 110–3600 m 2 s -1 . These mixing rates suggest a rapid transport mechanism for moving meltwater offshore. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctic Science Anvers Island Southern Ocean Cambridge University Press Antarctic Southern Ocean Antarctic Peninsula Anvers ENVELOPE(-63.500,-63.500,-64.600,-64.600) Anvers Island ENVELOPE(-63.500,-63.500,-64.600,-64.600) Antarctic Science 29 5 397 409 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
topic |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
spellingShingle |
Geology Ecology, Evolution, Behavior and Systematics Oceanography Corbett, D. Reide Crenshaw, Jared Null, Kimberly Peterson, Richard N. Peterson, Leigha E. Lyons, W. Berry Nearshore mixing and nutrient delivery along the western Antarctic Peninsula |
topic_facet |
Geology Ecology, Evolution, Behavior and Systematics Oceanography |
description |
Abstract The surface waters of the Southern Ocean play a key role in the global climate and carbon cycles by promoting growth of some of the world’s largest phytoplankton blooms. Several studies have emphasized the importance of glacial and sediment inputs of Fe that fuel the primary production of the Fe-limited Southern Ocean. Although the fertile surface waters along the shelf of the western Antarctic Peninsula (WAP) are influenced by large inputs of freshwater, this freshwater may take multiple pathways (e.g. calving, streams, groundwater discharge) with different degrees of water-rock interactions leading to variable Fe flux to coastal waters. During the summers of 2012–13 and 2013–14, seawater samples were collected along the WAP, near Anvers Island, to observe water column dynamics in nearshore and offshore waters. Tracers ( 223,224 Ra, 222 Rn, 18 O, 2 H) were used to evaluate the source and transport of water and nutrients in coastal fjords and across the shelf. Coastal waters are compared across two field seasons, with increased freshwater observed during 2014. Horizontal mixing rates of water masses along the WAP ranged from 110–3600 m 2 s -1 . These mixing rates suggest a rapid transport mechanism for moving meltwater offshore. |
format |
Article in Journal/Newspaper |
author |
Corbett, D. Reide Crenshaw, Jared Null, Kimberly Peterson, Richard N. Peterson, Leigha E. Lyons, W. Berry |
author_facet |
Corbett, D. Reide Crenshaw, Jared Null, Kimberly Peterson, Richard N. Peterson, Leigha E. Lyons, W. Berry |
author_sort |
Corbett, D. Reide |
title |
Nearshore mixing and nutrient delivery along the western Antarctic Peninsula |
title_short |
Nearshore mixing and nutrient delivery along the western Antarctic Peninsula |
title_full |
Nearshore mixing and nutrient delivery along the western Antarctic Peninsula |
title_fullStr |
Nearshore mixing and nutrient delivery along the western Antarctic Peninsula |
title_full_unstemmed |
Nearshore mixing and nutrient delivery along the western Antarctic Peninsula |
title_sort |
nearshore mixing and nutrient delivery along the western antarctic peninsula |
publisher |
Cambridge University Press (CUP) |
publishDate |
2017 |
url |
http://dx.doi.org/10.1017/s095410201700013x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201700013X |
long_lat |
ENVELOPE(-63.500,-63.500,-64.600,-64.600) ENVELOPE(-63.500,-63.500,-64.600,-64.600) |
geographic |
Antarctic Southern Ocean Antarctic Peninsula Anvers Anvers Island |
geographic_facet |
Antarctic Southern Ocean Antarctic Peninsula Anvers Anvers Island |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctic Science Anvers Island Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctic Science Anvers Island Southern Ocean |
op_source |
Antarctic Science volume 29, issue 5, page 397-409 ISSN 0954-1020 1365-2079 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1017/s095410201700013x |
container_title |
Antarctic Science |
container_volume |
29 |
container_issue |
5 |
container_start_page |
397 |
op_container_end_page |
409 |
_version_ |
1792505528107139072 |