Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay)

The processes contributing to the deep water renewal and oxygen balance of Pohja Bay are reviewed here, with reference to the extensive experimental material from the years 1990–1993. The observations reveal previously unreported frequent minor inflows of sea water into the bay. A one-dimensional di...

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Main Author: Stipa, T.
Format: Article in Journal/Newspaper
Language:English
Published: Boreal Environment Research Publishing Board 2024
Subjects:
Online Access:http://hdl.handle.net/10138/578066
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spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/578066 2024-09-15T18:00:08+00:00 Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay) Stipa, T. 2024-06-27T13:44:38Z 307-317 application/pdf http://hdl.handle.net/10138/578066 eng eng Boreal Environment Research Publishing Board Boreal Environment Research 1239-6095 1797-2469 4 http://hdl.handle.net/10138/578066 Suomen ympäristökeskus CC BY 4.0 openAccess Artikkeli lehdessä 2024 ftunivhelsihelda 2024-08-21T23:48:04Z The processes contributing to the deep water renewal and oxygen balance of Pohja Bay are reviewed here, with reference to the extensive experimental material from the years 1990–1993. The observations reveal previously unreported frequent minor inflows of sea water into the bay. A one-dimensional diffusion model is introduced and applied to computation of the diffusion-corrected biological oxygen sink during apparent deep water stagnation periods; the sink is evaluated as 0.06 ± 0.01 mg l–1 d–1. The results are summarized in a conceptual description of the physical processes underlying the estuarine circulation and oxygen balance of the bay. Article in Journal/Newspaper Boreal Environment Research HELDA – University of Helsinki Open Repository
institution Open Polar
collection HELDA – University of Helsinki Open Repository
op_collection_id ftunivhelsihelda
language English
description The processes contributing to the deep water renewal and oxygen balance of Pohja Bay are reviewed here, with reference to the extensive experimental material from the years 1990–1993. The observations reveal previously unreported frequent minor inflows of sea water into the bay. A one-dimensional diffusion model is introduced and applied to computation of the diffusion-corrected biological oxygen sink during apparent deep water stagnation periods; the sink is evaluated as 0.06 ± 0.01 mg l–1 d–1. The results are summarized in a conceptual description of the physical processes underlying the estuarine circulation and oxygen balance of the bay.
format Article in Journal/Newspaper
author Stipa, T.
spellingShingle Stipa, T.
Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay)
author_facet Stipa, T.
author_sort Stipa, T.
title Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay)
title_short Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay)
title_full Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay)
title_fullStr Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay)
title_full_unstemmed Water exchange and mixing in a semi-enclosed coastal basin (Pohja Bay)
title_sort water exchange and mixing in a semi-enclosed coastal basin (pohja bay)
publisher Boreal Environment Research Publishing Board
publishDate 2024
url http://hdl.handle.net/10138/578066
genre Boreal Environment Research
genre_facet Boreal Environment Research
op_relation Boreal Environment Research
1239-6095
1797-2469
4
http://hdl.handle.net/10138/578066
Suomen ympäristökeskus
op_rights CC BY 4.0
openAccess
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