Formation of nutrient rich bottom water in the eastern parth of the Barents Sea

During yearly routine observations of hydrography, nutrients and plankton in the Barents Sea we have observed a distinct anomaly in the distribution of the nutrients silicate and nitrate in near bottom water in an area off the west-southwest coast of Novaya Zemlya and in the eastern Barents Sea as a...

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Main Authors: Føyn, Lars, Hagebø, Magnar, Rey, Francisco, Seglem, Kjell
Format: Report
Language:English
Published: ICES 1997
Subjects:
Online Access:http://hdl.handle.net/11250/105755
id ftimr:oai:imr.brage.unit.no:11250/105755
record_format openpolar
spelling ftimr:oai:imr.brage.unit.no:11250/105755 2023-05-15T15:38:04+02:00 Formation of nutrient rich bottom water in the eastern parth of the Barents Sea Føyn, Lars Hagebø, Magnar Rey, Francisco Seglem, Kjell 1997 application/pdf http://hdl.handle.net/11250/105755 eng eng ICES ICES CM Documents;1997/R:1 This report is not to be cited without prior reference to the authors http://hdl.handle.net/11250/105755 8 s. currents strømforhold nutrient næringsstoffer hydrography hydrografi sampling prøvetaking VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497 VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 Working paper 1997 ftimr 2021-09-23T20:14:46Z During yearly routine observations of hydrography, nutrients and plankton in the Barents Sea we have observed a distinct anomaly in the distribution of the nutrients silicate and nitrate in near bottom water in an area off the west-southwest coast of Novaya Zemlya and in the eastern Barents Sea as a whole. Report Barents Sea Novaya Zemlya Institute for Marine Research: Brage IMR Barents Sea
institution Open Polar
collection Institute for Marine Research: Brage IMR
op_collection_id ftimr
language English
topic currents
strømforhold
nutrient
næringsstoffer
hydrography
hydrografi
sampling
prøvetaking
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
spellingShingle currents
strømforhold
nutrient
næringsstoffer
hydrography
hydrografi
sampling
prøvetaking
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
Føyn, Lars
Hagebø, Magnar
Rey, Francisco
Seglem, Kjell
Formation of nutrient rich bottom water in the eastern parth of the Barents Sea
topic_facet currents
strømforhold
nutrient
næringsstoffer
hydrography
hydrografi
sampling
prøvetaking
VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497
VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452
description During yearly routine observations of hydrography, nutrients and plankton in the Barents Sea we have observed a distinct anomaly in the distribution of the nutrients silicate and nitrate in near bottom water in an area off the west-southwest coast of Novaya Zemlya and in the eastern Barents Sea as a whole.
format Report
author Føyn, Lars
Hagebø, Magnar
Rey, Francisco
Seglem, Kjell
author_facet Føyn, Lars
Hagebø, Magnar
Rey, Francisco
Seglem, Kjell
author_sort Føyn, Lars
title Formation of nutrient rich bottom water in the eastern parth of the Barents Sea
title_short Formation of nutrient rich bottom water in the eastern parth of the Barents Sea
title_full Formation of nutrient rich bottom water in the eastern parth of the Barents Sea
title_fullStr Formation of nutrient rich bottom water in the eastern parth of the Barents Sea
title_full_unstemmed Formation of nutrient rich bottom water in the eastern parth of the Barents Sea
title_sort formation of nutrient rich bottom water in the eastern parth of the barents sea
publisher ICES
publishDate 1997
url http://hdl.handle.net/11250/105755
geographic Barents Sea
geographic_facet Barents Sea
genre Barents Sea
Novaya Zemlya
genre_facet Barents Sea
Novaya Zemlya
op_source 8 s.
op_relation ICES CM Documents;1997/R:1
This report is not to be cited without prior reference to the authors
http://hdl.handle.net/11250/105755
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