Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ...
The environment of the Fram Strait, the only deepwater connection of the Arctic Ocean to the world oceans via the North Atlantic (Fig.7.8.1; see Fig.7.1.9), is influenced by the distribution of sea-ice and two opposing current systems. The northward flowing West Spitsbergen Current (WSC) transports...
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ftdatacite:10.1594/pangaea.728140 2024-09-15T17:53:18+00:00 Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ... Birgel, Daniel Stein, Ruediger 2004 application/zip https://dx.doi.org/10.1594/pangaea.728140 https://doi.pangaea.de/10.1594/PANGAEA.728140 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Giant box corer Kasten corer Gravity corer Kiel type MultiCorer Multiple investigations ARK-XV/2 ARK-XVI/1 ARK-XVI/2 ARK-VIII/2 ARK-XIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo article Collection Supplementary Publication Series of Datasets 2004 ftdatacite https://doi.org/10.1594/pangaea.728140 2024-07-03T13:10:33Z The environment of the Fram Strait, the only deepwater connection of the Arctic Ocean to the world oceans via the North Atlantic (Fig.7.8.1; see Fig.7.1.9), is influenced by the distribution of sea-ice and two opposing current systems. The northward flowing West Spitsbergen Current (WSC) transports warm, near-surface water (Manley 1995; Rudels et al. 2000) to the Northern Fram Strait. About 22% of the northward flowing Atlantic waters are re-circulated within the RAC (Return Atlantic Current) between 78 and 80°N, west of Svalbard. At 80°N the WSC splits into the Svalbard (ca. 33% of the WSC waters) and the Yermak Branch (ca. 45% of the WSC waters). On the western side of the Fram Strait, the East Greenland Current (EGC) transports cold and low-salinity water southwards along the eastern continental margin of Greenland. (Fig.7.8.1).Primary production in ice-covered areas of western Fram Strait is limited by sea-ice cover, and influenced by the predominant water mass. Productivity in the interior Arctic Ocean ... : Supplement to: Birgel, Daniel; Stein, Ruediger (2004): Northern Fram Strait and Yermak Plateau: distribution, variability and burial of organic carbon and paleoenvironmental implications. In: Stein, R & Macdonald, R W (eds.), The Organic Carbon Cycle in the Arctic Ocean, Springer Verlag, Berlin, Heidelberg, New York, 279-294 ... Article in Journal/Newspaper Arctic Ocean East Greenland east greenland current Fram Strait Greenland North Atlantic Sea ice Svalbard Yermak plateau ice covered areas Spitsbergen DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Giant box corer Kasten corer Gravity corer Kiel type MultiCorer Multiple investigations ARK-XV/2 ARK-XVI/1 ARK-XVI/2 ARK-VIII/2 ARK-XIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
spellingShingle |
Giant box corer Kasten corer Gravity corer Kiel type MultiCorer Multiple investigations ARK-XV/2 ARK-XVI/1 ARK-XVI/2 ARK-VIII/2 ARK-XIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Birgel, Daniel Stein, Ruediger Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ... |
topic_facet |
Giant box corer Kasten corer Gravity corer Kiel type MultiCorer Multiple investigations ARK-XV/2 ARK-XVI/1 ARK-XVI/2 ARK-VIII/2 ARK-XIII/2 Polarstern Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo |
description |
The environment of the Fram Strait, the only deepwater connection of the Arctic Ocean to the world oceans via the North Atlantic (Fig.7.8.1; see Fig.7.1.9), is influenced by the distribution of sea-ice and two opposing current systems. The northward flowing West Spitsbergen Current (WSC) transports warm, near-surface water (Manley 1995; Rudels et al. 2000) to the Northern Fram Strait. About 22% of the northward flowing Atlantic waters are re-circulated within the RAC (Return Atlantic Current) between 78 and 80°N, west of Svalbard. At 80°N the WSC splits into the Svalbard (ca. 33% of the WSC waters) and the Yermak Branch (ca. 45% of the WSC waters). On the western side of the Fram Strait, the East Greenland Current (EGC) transports cold and low-salinity water southwards along the eastern continental margin of Greenland. (Fig.7.8.1).Primary production in ice-covered areas of western Fram Strait is limited by sea-ice cover, and influenced by the predominant water mass. Productivity in the interior Arctic Ocean ... : Supplement to: Birgel, Daniel; Stein, Ruediger (2004): Northern Fram Strait and Yermak Plateau: distribution, variability and burial of organic carbon and paleoenvironmental implications. In: Stein, R & Macdonald, R W (eds.), The Organic Carbon Cycle in the Arctic Ocean, Springer Verlag, Berlin, Heidelberg, New York, 279-294 ... |
format |
Article in Journal/Newspaper |
author |
Birgel, Daniel Stein, Ruediger |
author_facet |
Birgel, Daniel Stein, Ruediger |
author_sort |
Birgel, Daniel |
title |
Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ... |
title_short |
Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ... |
title_full |
Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ... |
title_fullStr |
Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ... |
title_full_unstemmed |
Distribution, variability and burial of organic carbon at Northern Fram Strait and Yermak Plateau ... |
title_sort |
distribution, variability and burial of organic carbon at northern fram strait and yermak plateau ... |
publisher |
PANGAEA |
publishDate |
2004 |
url |
https://dx.doi.org/10.1594/pangaea.728140 https://doi.pangaea.de/10.1594/PANGAEA.728140 |
genre |
Arctic Ocean East Greenland east greenland current Fram Strait Greenland North Atlantic Sea ice Svalbard Yermak plateau ice covered areas Spitsbergen |
genre_facet |
Arctic Ocean East Greenland east greenland current Fram Strait Greenland North Atlantic Sea ice Svalbard Yermak plateau ice covered areas Spitsbergen |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.728140 |
_version_ |
1810295328825409536 |