Tidal and residual currents in the Bransfield Strait, Antarctica

During the 1992-1993 oceanographic cruise of the Spanish R/V Hespérides, recording equipment was deployed in the Bransfield Strait. Six Aanderaa RCM7 current meters and three Aanderaa WLR7 tide gauges were successfully recovered after an operation period of 2.5 months. Relevant features of the time...

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Published in:Annales Geophysicae
Main Authors: López, O., García, M. A., S.-Arcilla, A.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.1007/s00585-994-0887-5
https://angeo.copernicus.org/articles/12/887/1994/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo33733 2023-05-15T13:31:38+02:00 Tidal and residual currents in the Bransfield Strait, Antarctica López, O. García, M. A. S.-Arcilla, A. 2018-09-27 application/pdf https://doi.org/10.1007/s00585-994-0887-5 https://angeo.copernicus.org/articles/12/887/1994/ eng eng doi:10.1007/s00585-994-0887-5 https://angeo.copernicus.org/articles/12/887/1994/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.1007/s00585-994-0887-5 2020-07-20T16:28:16Z During the 1992-1993 oceanographic cruise of the Spanish R/V Hespérides, recording equipment was deployed in the Bransfield Strait. Six Aanderaa RCM7 current meters and three Aanderaa WLR7 tide gauges were successfully recovered after an operation period of 2.5 months. Relevant features of the time series obtained are presented and discussed in this paper. The emphasis is placed on the tidal character of the currents and the relative importance of tidal flow in the general hydrodynamics of the strait. For these purposes a dense grid of hydrographic stations, completed during the BIOANTAR 93 cruise, is used. Preliminary geostrophic calculations relative to a 400 m depth, yield current velocities of around 0.20 m s -1 in the study area, whereas the magnitude of tidal currents is seen to be 0.30-0.40 m s -1 . Text Antarc* Antarctica Bransfield Strait Copernicus Publications: E-Journals Bransfield Strait Annales Geophysicae 12 9 887 902
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description During the 1992-1993 oceanographic cruise of the Spanish R/V Hespérides, recording equipment was deployed in the Bransfield Strait. Six Aanderaa RCM7 current meters and three Aanderaa WLR7 tide gauges were successfully recovered after an operation period of 2.5 months. Relevant features of the time series obtained are presented and discussed in this paper. The emphasis is placed on the tidal character of the currents and the relative importance of tidal flow in the general hydrodynamics of the strait. For these purposes a dense grid of hydrographic stations, completed during the BIOANTAR 93 cruise, is used. Preliminary geostrophic calculations relative to a 400 m depth, yield current velocities of around 0.20 m s -1 in the study area, whereas the magnitude of tidal currents is seen to be 0.30-0.40 m s -1 .
format Text
author López, O.
García, M. A.
S.-Arcilla, A.
spellingShingle López, O.
García, M. A.
S.-Arcilla, A.
Tidal and residual currents in the Bransfield Strait, Antarctica
author_facet López, O.
García, M. A.
S.-Arcilla, A.
author_sort López, O.
title Tidal and residual currents in the Bransfield Strait, Antarctica
title_short Tidal and residual currents in the Bransfield Strait, Antarctica
title_full Tidal and residual currents in the Bransfield Strait, Antarctica
title_fullStr Tidal and residual currents in the Bransfield Strait, Antarctica
title_full_unstemmed Tidal and residual currents in the Bransfield Strait, Antarctica
title_sort tidal and residual currents in the bransfield strait, antarctica
publishDate 2018
url https://doi.org/10.1007/s00585-994-0887-5
https://angeo.copernicus.org/articles/12/887/1994/
geographic Bransfield Strait
geographic_facet Bransfield Strait
genre Antarc*
Antarctica
Bransfield Strait
genre_facet Antarc*
Antarctica
Bransfield Strait
op_source eISSN: 1432-0576
op_relation doi:10.1007/s00585-994-0887-5
https://angeo.copernicus.org/articles/12/887/1994/
op_doi https://doi.org/10.1007/s00585-994-0887-5
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