Particle fluxes and composition at two mooring sites in the Polar Front Region ...
Particle fluxes and composition were examined over 5 years at two mooring sites in the Polar Front Region (site PF: 50°09.S, 5°50.E) and in the marginal winter sea-ice zone (site BO: 54°30.S, 3°20.W) in the eastern Atlantic Sector of the Southern Ocean. Seasonality, interannual variability and the m...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
2002
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.760873 https://doi.pangaea.de/10.1594/PANGAEA.760873 |
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author | Fischer, Gerhard Gersonde, Rainer Wefer, Gerold |
author_facet | Fischer, Gerhard Gersonde, Rainer Wefer, Gerold |
author_sort | Fischer, Gerhard |
collection | DataCite |
description | Particle fluxes and composition were examined over 5 years at two mooring sites in the Polar Front Region (site PF: 50°09.S, 5°50.E) and in the marginal winter sea-ice zone (site BO: 54°30.S, 3°20.W) in the eastern Atlantic Sector of the Southern Ocean. Seasonality, interannual variability and the magnitude of total mass fluxes were higher at site BO compared to PF. Five-year averages and standard deviations (1Sigma) of total mass fluxes were 19.6±18.5 and 24.8±29.9 g m**-2 at PF and BO, respectively. Peak fluxes at site BO occurred in January 1995, but the highest peak was measured in February 1991 (almost 1300 mg m**-2 d**-1) followed by post-bloom sedimentation in March through May. This would imply a time shift of several months between the onset of sea-ice retreat in October and major sedimentation events recorded in January/February with the upper BO traps. At site PF, highest fluxes of about 500 mg m**-2 d**-1 were found between December and March. Blooms at site BO, influenced by sea ice as indicated ... : Supplement to: Fischer, Gerhard; Gersonde, Rainer; Wefer, Gerold (2002): Organic carbon, biogenic silica and diatom fluxes in the marginal winter sea ice zone and in the Polar Front Region: interannual variation and changes in composition. Deep Sea Research Part II: Topical Studies in Oceanography, 49(9-10), 1721-1745 ... |
format | Article in Journal/Newspaper |
genre | Sea ice Southern Ocean |
genre_facet | Sea ice Southern Ocean |
geographic | Southern Ocean |
geographic_facet | Southern Ocean |
id | ftdatacite:10.1594/pangaea.760873 |
institution | Open Polar |
language | English |
op_collection_id | ftdatacite |
op_doi | https://doi.org/10.1594/pangaea.76087310.1016/s0967-0645(02)00009-7 |
op_relation | https://dx.doi.org/10.1016/s0967-0645(02)00009-7 |
op_rights | Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
publishDate | 2002 |
publisher | PANGAEA |
record_format | openpolar |
spelling | ftdatacite:10.1594/pangaea.760873 2025-01-17T00:43:38+00:00 Particle fluxes and composition at two mooring sites in the Polar Front Region ... Fischer, Gerhard Gersonde, Rainer Wefer, Gerold 2002 application/zip https://dx.doi.org/10.1594/pangaea.760873 https://doi.pangaea.de/10.1594/PANGAEA.760873 en eng PANGAEA https://dx.doi.org/10.1016/s0967-0645(02)00009-7 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Trap Mooring long time Mooring ANT-XII/2 ANT-V/4 ANT-XII/4 Polarstern Center for Marine Environmental Sciences MARUM article Supplementary Publication Series of Datasets Collection 2002 ftdatacite https://doi.org/10.1594/pangaea.76087310.1016/s0967-0645(02)00009-7 2024-04-02T11:56:27Z Particle fluxes and composition were examined over 5 years at two mooring sites in the Polar Front Region (site PF: 50°09.S, 5°50.E) and in the marginal winter sea-ice zone (site BO: 54°30.S, 3°20.W) in the eastern Atlantic Sector of the Southern Ocean. Seasonality, interannual variability and the magnitude of total mass fluxes were higher at site BO compared to PF. Five-year averages and standard deviations (1Sigma) of total mass fluxes were 19.6±18.5 and 24.8±29.9 g m**-2 at PF and BO, respectively. Peak fluxes at site BO occurred in January 1995, but the highest peak was measured in February 1991 (almost 1300 mg m**-2 d**-1) followed by post-bloom sedimentation in March through May. This would imply a time shift of several months between the onset of sea-ice retreat in October and major sedimentation events recorded in January/February with the upper BO traps. At site PF, highest fluxes of about 500 mg m**-2 d**-1 were found between December and March. Blooms at site BO, influenced by sea ice as indicated ... : Supplement to: Fischer, Gerhard; Gersonde, Rainer; Wefer, Gerold (2002): Organic carbon, biogenic silica and diatom fluxes in the marginal winter sea ice zone and in the Polar Front Region: interannual variation and changes in composition. Deep Sea Research Part II: Topical Studies in Oceanography, 49(9-10), 1721-1745 ... Article in Journal/Newspaper Sea ice Southern Ocean DataCite Southern Ocean |
spellingShingle | Trap Mooring long time Mooring ANT-XII/2 ANT-V/4 ANT-XII/4 Polarstern Center for Marine Environmental Sciences MARUM Fischer, Gerhard Gersonde, Rainer Wefer, Gerold Particle fluxes and composition at two mooring sites in the Polar Front Region ... |
title | Particle fluxes and composition at two mooring sites in the Polar Front Region ... |
title_full | Particle fluxes and composition at two mooring sites in the Polar Front Region ... |
title_fullStr | Particle fluxes and composition at two mooring sites in the Polar Front Region ... |
title_full_unstemmed | Particle fluxes and composition at two mooring sites in the Polar Front Region ... |
title_short | Particle fluxes and composition at two mooring sites in the Polar Front Region ... |
title_sort | particle fluxes and composition at two mooring sites in the polar front region ... |
topic | Trap Mooring long time Mooring ANT-XII/2 ANT-V/4 ANT-XII/4 Polarstern Center for Marine Environmental Sciences MARUM |
topic_facet | Trap Mooring long time Mooring ANT-XII/2 ANT-V/4 ANT-XII/4 Polarstern Center for Marine Environmental Sciences MARUM |
url | https://dx.doi.org/10.1594/pangaea.760873 https://doi.pangaea.de/10.1594/PANGAEA.760873 |