Study of tides and sea levels at Deception and Livingston islands, Antarctica

Abstract During the 2007–08 Spanish Antarctic campaign, two moorings of bottom pressure sensors were carried out over a ten week period. This paper presents the results of the tidal analysis from sea level records obtained at Deception and Livingston islands (South Shetland Islands, Antarctica). The...

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Published in:Antarctic Science
Main Authors: Vidal, Juan, Berrocoso, Manuel, Fernández-Ros, Alberto
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2011
Subjects:
Online Access:http://dx.doi.org/10.1017/s095410201100068x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201100068X
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spelling crcambridgeupr:10.1017/s095410201100068x 2024-09-15T17:48:40+00:00 Study of tides and sea levels at Deception and Livingston islands, Antarctica Vidal, Juan Berrocoso, Manuel Fernández-Ros, Alberto 2011 http://dx.doi.org/10.1017/s095410201100068x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201100068X en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 24, issue 2, page 193-201 ISSN 0954-1020 1365-2079 journal-article 2011 crcambridgeupr https://doi.org/10.1017/s095410201100068x 2024-07-31T04:04:10Z Abstract During the 2007–08 Spanish Antarctic campaign, two moorings of bottom pressure sensors were carried out over a ten week period. This paper presents the results of the tidal analysis from sea level records obtained at Deception and Livingston islands (South Shetland Islands, Antarctica). The main objective of this paper is to present a detailed study of the tidal characteristics at these two islands, for which statistical and harmonic analysis techniques are applied to the tidal records. A geodetic network was used to reference the pressure sensors. Geometric levelling, with an accuracy of 1 mm, allowed us to link the tidal marks with geodetic vertices located on Livingston and Deception islands. The amplitudes and phase lags obtained by harmonic analysis are compared to the harmonic constants of several coastal stations and co-tidal and co-range charts. Results show an evident influence of tides in the sea level signal, with a clear mixed semi-diurnal behaviour and a daily inequality between high and low waters. Measurements of salinity and temperature were made using electronic sensors. Results from this study showed that salinity and temperature were strongly influenced by tides. Seawater temperature varied in a manner that was consistent with the time series of residual bottom pressure. Article in Journal/Newspaper Antarc* Antarctic Antarctic Science Antarctica South Shetland Islands Cambridge University Press Antarctic Science 24 2 193 201
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract During the 2007–08 Spanish Antarctic campaign, two moorings of bottom pressure sensors were carried out over a ten week period. This paper presents the results of the tidal analysis from sea level records obtained at Deception and Livingston islands (South Shetland Islands, Antarctica). The main objective of this paper is to present a detailed study of the tidal characteristics at these two islands, for which statistical and harmonic analysis techniques are applied to the tidal records. A geodetic network was used to reference the pressure sensors. Geometric levelling, with an accuracy of 1 mm, allowed us to link the tidal marks with geodetic vertices located on Livingston and Deception islands. The amplitudes and phase lags obtained by harmonic analysis are compared to the harmonic constants of several coastal stations and co-tidal and co-range charts. Results show an evident influence of tides in the sea level signal, with a clear mixed semi-diurnal behaviour and a daily inequality between high and low waters. Measurements of salinity and temperature were made using electronic sensors. Results from this study showed that salinity and temperature were strongly influenced by tides. Seawater temperature varied in a manner that was consistent with the time series of residual bottom pressure.
format Article in Journal/Newspaper
author Vidal, Juan
Berrocoso, Manuel
Fernández-Ros, Alberto
spellingShingle Vidal, Juan
Berrocoso, Manuel
Fernández-Ros, Alberto
Study of tides and sea levels at Deception and Livingston islands, Antarctica
author_facet Vidal, Juan
Berrocoso, Manuel
Fernández-Ros, Alberto
author_sort Vidal, Juan
title Study of tides and sea levels at Deception and Livingston islands, Antarctica
title_short Study of tides and sea levels at Deception and Livingston islands, Antarctica
title_full Study of tides and sea levels at Deception and Livingston islands, Antarctica
title_fullStr Study of tides and sea levels at Deception and Livingston islands, Antarctica
title_full_unstemmed Study of tides and sea levels at Deception and Livingston islands, Antarctica
title_sort study of tides and sea levels at deception and livingston islands, antarctica
publisher Cambridge University Press (CUP)
publishDate 2011
url http://dx.doi.org/10.1017/s095410201100068x
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S095410201100068X
genre Antarc*
Antarctic
Antarctic Science
Antarctica
South Shetland Islands
genre_facet Antarc*
Antarctic
Antarctic Science
Antarctica
South Shetland Islands
op_source Antarctic Science
volume 24, issue 2, page 193-201
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s095410201100068x
container_title Antarctic Science
container_volume 24
container_issue 2
container_start_page 193
op_container_end_page 201
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