Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic

10. Davis Strait, Eastern Arctic Introductory presentation given at the 1st ATLAS General Assembly, June 2016. The Davis Strait joins two oceanic basins, Baffin Bay and the Labrador Sea, and separates western Greenland and Baffin Island. It connects to the Arctic Ocean in the north via the Baffin Ba...

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Main Author: Kenchington, Ellen
Format: Conference Object
Language:unknown
Published: Zenodo 2016
Subjects:
Online Access:https://dx.doi.org/10.5281/zenodo.376230
https://zenodo.org/record/376230
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spelling ftdatacite:10.5281/zenodo.376230 2023-05-15T14:51:57+02:00 Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic Kenchington, Ellen 2016 https://dx.doi.org/10.5281/zenodo.376230 https://zenodo.org/record/376230 unknown Zenodo Open Access Creative Commons Attribution 4.0 https://creativecommons.org/licenses/by/4.0 info:eu-repo/semantics/openAccess CC-BY Text Presentation article-journal ScholarlyArticle 2016 ftdatacite https://doi.org/10.5281/zenodo.376230 2021-11-05T12:55:41Z 10. Davis Strait, Eastern Arctic Introductory presentation given at the 1st ATLAS General Assembly, June 2016. The Davis Strait joins two oceanic basins, Baffin Bay and the Labrador Sea, and separates western Greenland and Baffin Island. It connects to the Arctic Ocean in the north via the Baffin Bay and to the Atlantic Ocean in the south via the Labrador Sea. It is considered to be the world's largest strait and is renowned for exceptionally strong tides, ranging from 9 to 18 m, and complex hydrography. The shelves extending from both Canada and Greenland typically range between 20 and 100 m in depth and are traversed by deep troughs. At its narrowest point, a ridge or sill up to approximately 600 m depth extends between Greenland (at Holsteinborg, Sisimiut) and Baffin Island (at Cape Dyer). The slopes along the Labrador Sea flank of this ridge and farther south along the Labrador and West Greenland shelves drop to 2500 m or more. On these slopes coral and sponge have been found, including the only known Lophelia pertusa reef in Greenlandic waters. South of Davis Strait the waters off west Greenland support intense phytoplankton blooms in April, which progress northward into the Baffin Bay in May as the seasonal ice-cover retreats. These blooms are characterised by high phytoplankton biomass and a community of grazers dominated by large copepods, i.e. Calanus . Within the study region Calanus provide an important food source for higher trophic levels ( e.g. fish, seabirds, whales). In addition, however, they play a key ecological role in supplying the benthic communities with high-quality food via the production of large and fast-sinking faecal pellets. The Baffin Bay and the Davis Strait have the only large-scale commercial fisheries in Canada's Arctic. Blue Growth Sectors: Biotechnology, Fisheries Conference Object Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin Island Baffin Cape Dyer Davis Strait Greenland greenlandic Labrador Sea Lophelia pertusa Phytoplankton Sisimiut Copepods DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Baffin Bay Baffin Island Canada Cape Dyer ENVELOPE(-61.573,-61.573,66.592,66.592) Dyer ENVELOPE(-81.366,-81.366,50.550,50.550) Greenland Sisimiut ENVELOPE(-53.674,-53.674,66.939,66.939)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
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description 10. Davis Strait, Eastern Arctic Introductory presentation given at the 1st ATLAS General Assembly, June 2016. The Davis Strait joins two oceanic basins, Baffin Bay and the Labrador Sea, and separates western Greenland and Baffin Island. It connects to the Arctic Ocean in the north via the Baffin Bay and to the Atlantic Ocean in the south via the Labrador Sea. It is considered to be the world's largest strait and is renowned for exceptionally strong tides, ranging from 9 to 18 m, and complex hydrography. The shelves extending from both Canada and Greenland typically range between 20 and 100 m in depth and are traversed by deep troughs. At its narrowest point, a ridge or sill up to approximately 600 m depth extends between Greenland (at Holsteinborg, Sisimiut) and Baffin Island (at Cape Dyer). The slopes along the Labrador Sea flank of this ridge and farther south along the Labrador and West Greenland shelves drop to 2500 m or more. On these slopes coral and sponge have been found, including the only known Lophelia pertusa reef in Greenlandic waters. South of Davis Strait the waters off west Greenland support intense phytoplankton blooms in April, which progress northward into the Baffin Bay in May as the seasonal ice-cover retreats. These blooms are characterised by high phytoplankton biomass and a community of grazers dominated by large copepods, i.e. Calanus . Within the study region Calanus provide an important food source for higher trophic levels ( e.g. fish, seabirds, whales). In addition, however, they play a key ecological role in supplying the benthic communities with high-quality food via the production of large and fast-sinking faecal pellets. The Baffin Bay and the Davis Strait have the only large-scale commercial fisheries in Canada's Arctic. Blue Growth Sectors: Biotechnology, Fisheries
format Conference Object
author Kenchington, Ellen
spellingShingle Kenchington, Ellen
Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic
author_facet Kenchington, Ellen
author_sort Kenchington, Ellen
title Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic
title_short Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic
title_full Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic
title_fullStr Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic
title_full_unstemmed Introduction To Atlas Case Study 10: Davis Strait, Eastern Arctic
title_sort introduction to atlas case study 10: davis strait, eastern arctic
publisher Zenodo
publishDate 2016
url https://dx.doi.org/10.5281/zenodo.376230
https://zenodo.org/record/376230
long_lat ENVELOPE(-61.573,-61.573,66.592,66.592)
ENVELOPE(-81.366,-81.366,50.550,50.550)
ENVELOPE(-53.674,-53.674,66.939,66.939)
geographic Arctic
Arctic Ocean
Baffin Bay
Baffin Island
Canada
Cape Dyer
Dyer
Greenland
Sisimiut
geographic_facet Arctic
Arctic Ocean
Baffin Bay
Baffin Island
Canada
Cape Dyer
Dyer
Greenland
Sisimiut
genre Arctic
Arctic Ocean
Baffin Bay
Baffin Bay
Baffin Island
Baffin
Cape Dyer
Davis Strait
Greenland
greenlandic
Labrador Sea
Lophelia pertusa
Phytoplankton
Sisimiut
Copepods
genre_facet Arctic
Arctic Ocean
Baffin Bay
Baffin Bay
Baffin Island
Baffin
Cape Dyer
Davis Strait
Greenland
greenlandic
Labrador Sea
Lophelia pertusa
Phytoplankton
Sisimiut
Copepods
op_rights Open Access
Creative Commons Attribution 4.0
https://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.5281/zenodo.376230
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