Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer

An analysis of suspended particulate matter (SPM) and phytoplankton distribution, composition and vertical particle fluxes in Russkaya Gavan’ Bay (Northern Island of the Novaya Zemlya), Bezymyannaya Bay (Southern Island of the Novaya Zemlya), Dolgaya Bay (northwestern part of the Vaigach Island) in...

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Published in:Advances in Meteorology
Main Authors: N. V. Politova, V. P. Shevchenko, V. V. Zernova
Format: Article in Journal/Newspaper
Language:English
Published: Advances in Meteorology 2012
Subjects:
Online Access:https://doi.org/10.1155/2012/259316
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spelling fthindawi:oai:hindawi.com:10.1155/2012/259316 2023-05-15T15:38:59+02:00 Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer N. V. Politova V. P. Shevchenko V. V. Zernova 2012 https://doi.org/10.1155/2012/259316 en eng Advances in Meteorology https://doi.org/10.1155/2012/259316 Copyright © 2012 N. V. Politova et al. Research Article 2012 fthindawi https://doi.org/10.1155/2012/259316 2019-05-25T23:29:55Z An analysis of suspended particulate matter (SPM) and phytoplankton distribution, composition and vertical particle fluxes in Russkaya Gavan’ Bay (Northern Island of the Novaya Zemlya), Bezymyannaya Bay (Southern Island of the Novaya Zemlya), Dolgaya Bay (northwestern part of the Vaigach Island) in comparison with the data from the Svalbard Archipelago is presented. Field studies were carried out by the authors during the 9th expedition of the RV “Professor Logachev” in September 1994, the 11th, 13th, and 14th expeditions of the RV “Akademik Sergey Vavilov” in September-October 1997 and August-September 1998. The data about Spitsbergen fjords are from literature. Our results show that, on the bays of the Barents Sea islands, most SPM stays in the bays (fjords) and only small part of it reaches the open sea. This is due to the hydrodynamic conditions in the bays, the large size of the particles, flocculation, and often to the morphological barriers in the relief at the bay entrances. It is important for ecological purposes to map out migration pathways of the SPM with pollutants from bays to the open sea. Results of our investigation indicate that the western bays of the Novaya Zemlya act as traps for SPM derived from glaciers and coastal abrasion. Article in Journal/Newspaper Barents Sea Novaya Zemlya Svalbard Spitsbergen Hindawi Publishing Corporation Barents Sea Dolgaya ENVELOPE(82.694,82.694,71.892,71.892) Russkaya ENVELOPE(159.362,159.362,63.593,63.593) Southern Island ENVELOPE(-55.577,-55.577,52.266,52.266) Svalbard Svalbard Archipelago Advances in Meteorology 2012 1 15
institution Open Polar
collection Hindawi Publishing Corporation
op_collection_id fthindawi
language English
description An analysis of suspended particulate matter (SPM) and phytoplankton distribution, composition and vertical particle fluxes in Russkaya Gavan’ Bay (Northern Island of the Novaya Zemlya), Bezymyannaya Bay (Southern Island of the Novaya Zemlya), Dolgaya Bay (northwestern part of the Vaigach Island) in comparison with the data from the Svalbard Archipelago is presented. Field studies were carried out by the authors during the 9th expedition of the RV “Professor Logachev” in September 1994, the 11th, 13th, and 14th expeditions of the RV “Akademik Sergey Vavilov” in September-October 1997 and August-September 1998. The data about Spitsbergen fjords are from literature. Our results show that, on the bays of the Barents Sea islands, most SPM stays in the bays (fjords) and only small part of it reaches the open sea. This is due to the hydrodynamic conditions in the bays, the large size of the particles, flocculation, and often to the morphological barriers in the relief at the bay entrances. It is important for ecological purposes to map out migration pathways of the SPM with pollutants from bays to the open sea. Results of our investigation indicate that the western bays of the Novaya Zemlya act as traps for SPM derived from glaciers and coastal abrasion.
format Article in Journal/Newspaper
author N. V. Politova
V. P. Shevchenko
V. V. Zernova
spellingShingle N. V. Politova
V. P. Shevchenko
V. V. Zernova
Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer
author_facet N. V. Politova
V. P. Shevchenko
V. V. Zernova
author_sort N. V. Politova
title Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer
title_short Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer
title_full Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer
title_fullStr Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer
title_full_unstemmed Distribution, Composition, and Vertical Fluxes of Particulate Matter in Bays of Novaya Zemlya Archipelago, Vaigach Island at the End of Summer
title_sort distribution, composition, and vertical fluxes of particulate matter in bays of novaya zemlya archipelago, vaigach island at the end of summer
publisher Advances in Meteorology
publishDate 2012
url https://doi.org/10.1155/2012/259316
long_lat ENVELOPE(82.694,82.694,71.892,71.892)
ENVELOPE(159.362,159.362,63.593,63.593)
ENVELOPE(-55.577,-55.577,52.266,52.266)
geographic Barents Sea
Dolgaya
Russkaya
Southern Island
Svalbard
Svalbard Archipelago
geographic_facet Barents Sea
Dolgaya
Russkaya
Southern Island
Svalbard
Svalbard Archipelago
genre Barents Sea
Novaya Zemlya
Svalbard
Spitsbergen
genre_facet Barents Sea
Novaya Zemlya
Svalbard
Spitsbergen
op_relation https://doi.org/10.1155/2012/259316
op_rights Copyright © 2012 N. V. Politova et al.
op_doi https://doi.org/10.1155/2012/259316
container_title Advances in Meteorology
container_volume 2012
container_start_page 1
op_container_end_page 15
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