Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring

In spring of 2016, 2018 and 2019, chlorophyll a (Chl a) content was studied in the 0-50 m layer on the vast Barents Sea area - to the north of 75∘ N. Standard sampling was carried out at 11 oceanographic transects, including 52 stations. Due to the negative ice anomalies and the high-latitude positi...

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Main Authors: Makarevich, P. (Pavel), Vodopianova, V. (Veronika), Bulavina, A. (Aleksandra), Kalinka, O. (Olga)
Format: Other/Unknown Material
Language:Indonesian
Published: Knowledge E 2020
Subjects:
Online Access:https://www.neliti.com/publications/511883/influence-of-the-barents-sea-frontal-zones-on-chlorophyll-concentration-in-sprin
id ftneliti:oai:neliti.com:511883
record_format openpolar
spelling ftneliti:oai:neliti.com:511883 2023-05-15T14:39:34+02:00 Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring Makarevich, P. (Pavel) Vodopianova, V. (Veronika) Bulavina, A. (Aleksandra) Kalinka, O. (Olga) 2020-01-15 application/pdf https://www.neliti.com/publications/511883/influence-of-the-barents-sea-frontal-zones-on-chlorophyll-concentration-in-sprin id ind Knowledge E https://www.neliti.com/publications/511883/influence-of-the-barents-sea-frontal-zones-on-chlorophyll-concentration-in-sprin (c) KnE Life Sciences, 2020 KnE Life Sciences Indonesia Journal:eArticle 2020 ftneliti 2022-10-19T04:21:13Z In spring of 2016, 2018 and 2019, chlorophyll a (Chl a) content was studied in the 0-50 m layer on the vast Barents Sea area - to the north of 75∘ N. Standard sampling was carried out at 11 oceanographic transects, including 52 stations. Due to the negative ice anomalies and the high-latitude position of the ice edge, original data on Chl a concentration for spring period were obtained in hard-to-reach and previously unexplored areas of the Barents Sea. The investigation area covered the Marginal Ice Arctic zone, as well as the area where the Polar Front was located quasi-stationary. The effect of the Marginal Ice Arctic and Polar frontal zones on the distribution of Chl a concentration was revealed. The strongest factor influencing the distribution of chlorophyll was the Polar Front. It divided mainly Arctic and Atlantic waters. The highest pigment concentrations corresponded to the Arctic water mass and exceeded the content of pigment in water of Atlantic origin by an order of magnitude. The impact of the Marginal Ice Arctic Front was not so obvious - the content of Chl a in waters of various genesis differed, but not more than by a factor of 2. Other/Unknown Material Arctic Barents Sea neliti (Indonesia's Think Tank Database) Arctic Barents Sea
institution Open Polar
collection neliti (Indonesia's Think Tank Database)
op_collection_id ftneliti
language Indonesian
topic Indonesia
spellingShingle Indonesia
Makarevich, P. (Pavel)
Vodopianova, V. (Veronika)
Bulavina, A. (Aleksandra)
Kalinka, O. (Olga)
Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring
topic_facet Indonesia
description In spring of 2016, 2018 and 2019, chlorophyll a (Chl a) content was studied in the 0-50 m layer on the vast Barents Sea area - to the north of 75∘ N. Standard sampling was carried out at 11 oceanographic transects, including 52 stations. Due to the negative ice anomalies and the high-latitude position of the ice edge, original data on Chl a concentration for spring period were obtained in hard-to-reach and previously unexplored areas of the Barents Sea. The investigation area covered the Marginal Ice Arctic zone, as well as the area where the Polar Front was located quasi-stationary. The effect of the Marginal Ice Arctic and Polar frontal zones on the distribution of Chl a concentration was revealed. The strongest factor influencing the distribution of chlorophyll was the Polar Front. It divided mainly Arctic and Atlantic waters. The highest pigment concentrations corresponded to the Arctic water mass and exceeded the content of pigment in water of Atlantic origin by an order of magnitude. The impact of the Marginal Ice Arctic Front was not so obvious - the content of Chl a in waters of various genesis differed, but not more than by a factor of 2.
format Other/Unknown Material
author Makarevich, P. (Pavel)
Vodopianova, V. (Veronika)
Bulavina, A. (Aleksandra)
Kalinka, O. (Olga)
author_facet Makarevich, P. (Pavel)
Vodopianova, V. (Veronika)
Bulavina, A. (Aleksandra)
Kalinka, O. (Olga)
author_sort Makarevich, P. (Pavel)
title Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring
title_short Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring
title_full Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring
title_fullStr Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring
title_full_unstemmed Influence of the Barents Sea Frontal Zones on Chlorophyll Concentration in Spring
title_sort influence of the barents sea frontal zones on chlorophyll concentration in spring
publisher Knowledge E
publishDate 2020
url https://www.neliti.com/publications/511883/influence-of-the-barents-sea-frontal-zones-on-chlorophyll-concentration-in-sprin
geographic Arctic
Barents Sea
geographic_facet Arctic
Barents Sea
genre Arctic
Barents Sea
genre_facet Arctic
Barents Sea
op_source KnE Life Sciences
op_relation https://www.neliti.com/publications/511883/influence-of-the-barents-sea-frontal-zones-on-chlorophyll-concentration-in-sprin
op_rights (c) KnE Life Sciences, 2020
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