Hydrodynamic modelling of Port Foster, Deception Island, Antarctica

Abstract Over the last decade, the Antarctic continent has been the object of intensive scientific programmes. However, the emphasis of these studies rarely focuses on the Antarctic as a source of potential elements such as mercury. The release of mercury to the environment is known to occur at Dece...

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Published in:Antarctic Science
Main Authors: Figueiredo, Daniel, Dos Santos, Aires, Mateus, Marcos, Pinto, Ligia
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2017
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102017000463
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102017000463
id crcambridgeupr:10.1017/s0954102017000463
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spelling crcambridgeupr:10.1017/s0954102017000463 2024-03-03T08:38:36+00:00 Hydrodynamic modelling of Port Foster, Deception Island, Antarctica Figueiredo, Daniel Dos Santos, Aires Mateus, Marcos Pinto, Ligia 2017 http://dx.doi.org/10.1017/s0954102017000463 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102017000463 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 30, issue 2, page 115-124 ISSN 0954-1020 1365-2079 Geology Ecology, Evolution, Behavior and Systematics Oceanography journal-article 2017 crcambridgeupr https://doi.org/10.1017/s0954102017000463 2024-02-08T08:47:21Z Abstract Over the last decade, the Antarctic continent has been the object of intensive scientific programmes. However, the emphasis of these studies rarely focuses on the Antarctic as a source of potential elements such as mercury. The release of mercury to the environment is known to occur at Deception Island, associated with volcanic activity. In this study, a 3D hydrodynamic model was used to assess the role of water circulation on the dispersion of released mercury. Sea level variation and tidal circulation data were obtained. Residence time was calculated using two different approaches. Internal tide generation in summer and winter were recognized and the barotropic tidal components obtained. Lagrangian tracers were used to depict particle circulation (simulating particulate mercury) in a three month summer simulation for barotropic and baroclinic conditions. The results show that particles accumulate in the northern and western parts of the bay. It is acknowledged that the results of the 3D model are associated with a non-negligible uncertainty, which can only be reduced with an ongoing commitment to monitoring. The findings of this study indicate that mercury accumulation is occurring in Port Foster (Deception Island), which is a potential threat to the local ecosystem. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Antarctica Deception Island Cambridge University Press Antarctic The Antarctic Deception Island ENVELOPE(-60.633,-60.633,-62.950,-62.950) Port Foster ENVELOPE(162.967,162.967,-78.400,-78.400) Antarctic Science 30 2 115 124
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
spellingShingle Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
Figueiredo, Daniel
Dos Santos, Aires
Mateus, Marcos
Pinto, Ligia
Hydrodynamic modelling of Port Foster, Deception Island, Antarctica
topic_facet Geology
Ecology, Evolution, Behavior and Systematics
Oceanography
description Abstract Over the last decade, the Antarctic continent has been the object of intensive scientific programmes. However, the emphasis of these studies rarely focuses on the Antarctic as a source of potential elements such as mercury. The release of mercury to the environment is known to occur at Deception Island, associated with volcanic activity. In this study, a 3D hydrodynamic model was used to assess the role of water circulation on the dispersion of released mercury. Sea level variation and tidal circulation data were obtained. Residence time was calculated using two different approaches. Internal tide generation in summer and winter were recognized and the barotropic tidal components obtained. Lagrangian tracers were used to depict particle circulation (simulating particulate mercury) in a three month summer simulation for barotropic and baroclinic conditions. The results show that particles accumulate in the northern and western parts of the bay. It is acknowledged that the results of the 3D model are associated with a non-negligible uncertainty, which can only be reduced with an ongoing commitment to monitoring. The findings of this study indicate that mercury accumulation is occurring in Port Foster (Deception Island), which is a potential threat to the local ecosystem.
format Article in Journal/Newspaper
author Figueiredo, Daniel
Dos Santos, Aires
Mateus, Marcos
Pinto, Ligia
author_facet Figueiredo, Daniel
Dos Santos, Aires
Mateus, Marcos
Pinto, Ligia
author_sort Figueiredo, Daniel
title Hydrodynamic modelling of Port Foster, Deception Island, Antarctica
title_short Hydrodynamic modelling of Port Foster, Deception Island, Antarctica
title_full Hydrodynamic modelling of Port Foster, Deception Island, Antarctica
title_fullStr Hydrodynamic modelling of Port Foster, Deception Island, Antarctica
title_full_unstemmed Hydrodynamic modelling of Port Foster, Deception Island, Antarctica
title_sort hydrodynamic modelling of port foster, deception island, antarctica
publisher Cambridge University Press (CUP)
publishDate 2017
url http://dx.doi.org/10.1017/s0954102017000463
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102017000463
long_lat ENVELOPE(-60.633,-60.633,-62.950,-62.950)
ENVELOPE(162.967,162.967,-78.400,-78.400)
geographic Antarctic
The Antarctic
Deception Island
Port Foster
geographic_facet Antarctic
The Antarctic
Deception Island
Port Foster
genre Antarc*
Antarctic
Antarctic Science
Antarctica
Deception Island
genre_facet Antarc*
Antarctic
Antarctic Science
Antarctica
Deception Island
op_source Antarctic Science
volume 30, issue 2, page 115-124
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102017000463
container_title Antarctic Science
container_volume 30
container_issue 2
container_start_page 115
op_container_end_page 124
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