Surface currents in the Porsanger fjord in northern Norway
We describe surface currents in the Porsanger fjord (Porsangerfjorden) located in the European Arctic in the vicinity of the Barents Sea. Our analysis is based on surface current data collected in the summer of 2014 using High Frequency (WERA, Helzel Messtechnik GmbH) radar system. One of our object...
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Polish Academy of Sciences
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ftdoajarticles:oai:doaj.org/article:6aad67efbff747859e626e152299b39d 2023-05-15T14:58:40+02:00 Surface currents in the Porsanger fjord in northern Norway Stramska Malgorzata Jankowski Andrzej Cieszyńska Agata 2016-09-01T00:00:00Z https://doi.org/10.1515/popore-2016-0018 https://doaj.org/article/6aad67efbff747859e626e152299b39d EN eng Polish Academy of Sciences http://www.degruyter.com/view/j/popore.2016.37.issue-3/popore-2016-0018/popore-2016-0018.xml?format=INT https://doaj.org/toc/2081-8262 2081-8262 doi:10.1515/popore-2016-0018 https://doaj.org/article/6aad67efbff747859e626e152299b39d Polish Polar Research, Vol 37, Iss 3, Pp 337-360 (2016) Arctic northern Norway fjords coastal processes tides ocean observing systems Geology QE1-996.5 article 2016 ftdoajarticles https://doi.org/10.1515/popore-2016-0018 2022-12-31T16:33:57Z We describe surface currents in the Porsanger fjord (Porsangerfjorden) located in the European Arctic in the vicinity of the Barents Sea. Our analysis is based on surface current data collected in the summer of 2014 using High Frequency (WERA, Helzel Messtechnik GmbH) radar system. One of our objectives was to separate out the tidal from the nontidal components of the currents and to determine the most important tidal constituents. Tides in the Porsanger fjord are substantial, with tidal range on the order of about 3 m. Tidal analysis attributes to tides about 99% of variance in sea level time series recorded in Honningsvaag. The most important tidal component in sea level data is the M2 component, with amplitude of ~90 cm. The S2 and N2 constituents (amplitude of ~20 cm) also play a significant role in the semidiurnal sea level oscillations. The most important diurnal component is K1 with amplitude of about 8 cm. The most important tidal component in analyzed surface currents records is the M2 component. The second most important component is the S2. Our results indicate that in contrast to sea level, only about 10-30% of variance in surface currents can be attributed to tidal currents. This means that about 70-90% of variance is due to wind-induced and geostrophic currents. Article in Journal/Newspaper Arctic Barents Sea Northern Norway Polar Research Porsangerfjorden Directory of Open Access Journals: DOAJ Articles Arctic Barents Sea Norway Porsanger ENVELOPE(24.956,24.956,70.052,70.052) Polish Polar Research 37 3 337 360 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Arctic northern Norway fjords coastal processes tides ocean observing systems Geology QE1-996.5 |
spellingShingle |
Arctic northern Norway fjords coastal processes tides ocean observing systems Geology QE1-996.5 Stramska Malgorzata Jankowski Andrzej Cieszyńska Agata Surface currents in the Porsanger fjord in northern Norway |
topic_facet |
Arctic northern Norway fjords coastal processes tides ocean observing systems Geology QE1-996.5 |
description |
We describe surface currents in the Porsanger fjord (Porsangerfjorden) located in the European Arctic in the vicinity of the Barents Sea. Our analysis is based on surface current data collected in the summer of 2014 using High Frequency (WERA, Helzel Messtechnik GmbH) radar system. One of our objectives was to separate out the tidal from the nontidal components of the currents and to determine the most important tidal constituents. Tides in the Porsanger fjord are substantial, with tidal range on the order of about 3 m. Tidal analysis attributes to tides about 99% of variance in sea level time series recorded in Honningsvaag. The most important tidal component in sea level data is the M2 component, with amplitude of ~90 cm. The S2 and N2 constituents (amplitude of ~20 cm) also play a significant role in the semidiurnal sea level oscillations. The most important diurnal component is K1 with amplitude of about 8 cm. The most important tidal component in analyzed surface currents records is the M2 component. The second most important component is the S2. Our results indicate that in contrast to sea level, only about 10-30% of variance in surface currents can be attributed to tidal currents. This means that about 70-90% of variance is due to wind-induced and geostrophic currents. |
format |
Article in Journal/Newspaper |
author |
Stramska Malgorzata Jankowski Andrzej Cieszyńska Agata |
author_facet |
Stramska Malgorzata Jankowski Andrzej Cieszyńska Agata |
author_sort |
Stramska Malgorzata |
title |
Surface currents in the Porsanger fjord in northern Norway |
title_short |
Surface currents in the Porsanger fjord in northern Norway |
title_full |
Surface currents in the Porsanger fjord in northern Norway |
title_fullStr |
Surface currents in the Porsanger fjord in northern Norway |
title_full_unstemmed |
Surface currents in the Porsanger fjord in northern Norway |
title_sort |
surface currents in the porsanger fjord in northern norway |
publisher |
Polish Academy of Sciences |
publishDate |
2016 |
url |
https://doi.org/10.1515/popore-2016-0018 https://doaj.org/article/6aad67efbff747859e626e152299b39d |
long_lat |
ENVELOPE(24.956,24.956,70.052,70.052) |
geographic |
Arctic Barents Sea Norway Porsanger |
geographic_facet |
Arctic Barents Sea Norway Porsanger |
genre |
Arctic Barents Sea Northern Norway Polar Research Porsangerfjorden |
genre_facet |
Arctic Barents Sea Northern Norway Polar Research Porsangerfjorden |
op_source |
Polish Polar Research, Vol 37, Iss 3, Pp 337-360 (2016) |
op_relation |
http://www.degruyter.com/view/j/popore.2016.37.issue-3/popore-2016-0018/popore-2016-0018.xml?format=INT https://doaj.org/toc/2081-8262 2081-8262 doi:10.1515/popore-2016-0018 https://doaj.org/article/6aad67efbff747859e626e152299b39d |
op_doi |
https://doi.org/10.1515/popore-2016-0018 |
container_title |
Polish Polar Research |
container_volume |
37 |
container_issue |
3 |
container_start_page |
337 |
op_container_end_page |
360 |
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1766330791030161408 |