Constraining energetic slope currents through assimilation of high-frequency radar observations

Assimilation of high-frequency (HF) radar current observations and CTD hydrography is performed with the 4D-Var analysis scheme implemented in the Regional Ocean Modeling System (ROMS). We consider both an idealized case, with a baroclinic slope current in a periodic channel, and a realistic case fo...

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Published in:Ocean Science
Main Authors: Sperrevik, Ann Kristin, Christensen, Kai Håkon, Röhrs, Johannes
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2015
Subjects:
Online Access:https://hdl.handle.net/1956/16173
https://doi.org/10.5194/os-11-237-2015
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spelling ftunivbergen:oai:bora.uib.no:1956/16173 2023-05-15T17:43:26+02:00 Constraining energetic slope currents through assimilation of high-frequency radar observations Sperrevik, Ann Kristin Christensen, Kai Håkon Röhrs, Johannes 2015-03-11 application/pdf https://hdl.handle.net/1956/16173 https://doi.org/10.5194/os-11-237-2015 eng eng Copernicus Modeling coastal circulation in Norway using a high-resolution 4D-Var ocean assimilation system urn:issn:1812-0784 https://hdl.handle.net/1956/16173 https://doi.org/10.5194/os-11-237-2015 cristin:1340314 Attribution CC BY http://creativecommons.org/licenses/by/3.0/ Copyright 2015 The Authors Ocean Science 11 2 237-249 Peer reviewed Journal article 2015 ftunivbergen https://doi.org/10.5194/os-11-237-2015 2023-03-14T17:42:10Z Assimilation of high-frequency (HF) radar current observations and CTD hydrography is performed with the 4D-Var analysis scheme implemented in the Regional Ocean Modeling System (ROMS). We consider both an idealized case, with a baroclinic slope current in a periodic channel, and a realistic case for the coast of Vesterålen in northern Norway. In the realistic case, the results of the data assimilation are compared with independent data from acoustic profilers and surface drifters. Best results are obtained when background error correlation scales are small (10 km or less) and when the data assimilation window is short, i.e. about 1 day. Furthermore, we find that the impact of assimilating HF radar currents is generally larger than the impact of CTD hydrography. However, combining the HF radar currents with a few hydrographic profiles gives significantly better results, which demonstrates the importance of complementing surface observations with observations of the vertical structure of the ocean. publishedVersion Article in Journal/Newspaper Northern Norway Vesterålen University of Bergen: Bergen Open Research Archive (BORA-UiB) Norway Vesterålen ENVELOPE(14.939,14.939,68.754,68.754) Ocean Science 11 2 237 249
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
description Assimilation of high-frequency (HF) radar current observations and CTD hydrography is performed with the 4D-Var analysis scheme implemented in the Regional Ocean Modeling System (ROMS). We consider both an idealized case, with a baroclinic slope current in a periodic channel, and a realistic case for the coast of Vesterålen in northern Norway. In the realistic case, the results of the data assimilation are compared with independent data from acoustic profilers and surface drifters. Best results are obtained when background error correlation scales are small (10 km or less) and when the data assimilation window is short, i.e. about 1 day. Furthermore, we find that the impact of assimilating HF radar currents is generally larger than the impact of CTD hydrography. However, combining the HF radar currents with a few hydrographic profiles gives significantly better results, which demonstrates the importance of complementing surface observations with observations of the vertical structure of the ocean. publishedVersion
format Article in Journal/Newspaper
author Sperrevik, Ann Kristin
Christensen, Kai Håkon
Röhrs, Johannes
spellingShingle Sperrevik, Ann Kristin
Christensen, Kai Håkon
Röhrs, Johannes
Constraining energetic slope currents through assimilation of high-frequency radar observations
author_facet Sperrevik, Ann Kristin
Christensen, Kai Håkon
Röhrs, Johannes
author_sort Sperrevik, Ann Kristin
title Constraining energetic slope currents through assimilation of high-frequency radar observations
title_short Constraining energetic slope currents through assimilation of high-frequency radar observations
title_full Constraining energetic slope currents through assimilation of high-frequency radar observations
title_fullStr Constraining energetic slope currents through assimilation of high-frequency radar observations
title_full_unstemmed Constraining energetic slope currents through assimilation of high-frequency radar observations
title_sort constraining energetic slope currents through assimilation of high-frequency radar observations
publisher Copernicus
publishDate 2015
url https://hdl.handle.net/1956/16173
https://doi.org/10.5194/os-11-237-2015
long_lat ENVELOPE(14.939,14.939,68.754,68.754)
geographic Norway
Vesterålen
geographic_facet Norway
Vesterålen
genre Northern Norway
Vesterålen
genre_facet Northern Norway
Vesterålen
op_source Ocean Science
11
2
237-249
op_relation Modeling coastal circulation in Norway using a high-resolution 4D-Var ocean assimilation system
urn:issn:1812-0784
https://hdl.handle.net/1956/16173
https://doi.org/10.5194/os-11-237-2015
cristin:1340314
op_rights Attribution CC BY
http://creativecommons.org/licenses/by/3.0/
Copyright 2015 The Authors
op_doi https://doi.org/10.5194/os-11-237-2015
container_title Ocean Science
container_volume 11
container_issue 2
container_start_page 237
op_container_end_page 249
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