Polar outflow from the Arctic Ocean: A high resolution model study

Arctic fresh water plays a large role in both the global ocean circulation and the hydrological cycle. To identify sources and pathways of the Arctic outflow into the North Atlantic, results of a high resolution global model and observations have been examined. It is shown that continental runoff an...

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Published in:Journal of Marine Systems
Main Authors: Aksenov, Yevgeny, Bacon, Sheldon, Coward, Andrew C., Holliday, N. Penny
Format: Article in Journal/Newspaper
Language:unknown
Published: 2010
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/264033/
https://doi.org/10.1016/j.jmarsys.2010.06.007
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spelling ftnerc:oai:nora.nerc.ac.uk:264033 2023-05-15T14:26:44+02:00 Polar outflow from the Arctic Ocean: A high resolution model study Aksenov, Yevgeny Bacon, Sheldon Coward, Andrew C. Holliday, N. Penny 2010-10 http://nora.nerc.ac.uk/id/eprint/264033/ https://doi.org/10.1016/j.jmarsys.2010.06.007 unknown Aksenov, Yevgeny orcid:0000-0001-6132-3434 Bacon, Sheldon orcid:0000-0002-2471-9373 Coward, Andrew C. orcid:0000-0002-9111-7700 Holliday, N. Penny orcid:0000-0002-9733-8002 . 2010 Polar outflow from the Arctic Ocean: A high resolution model study. Journal of Marine Systems, 83 (1-2). 14-37. https://doi.org/10.1016/j.jmarsys.2010.06.007 <https://doi.org/10.1016/j.jmarsys.2010.06.007> Publication - Article PeerReviewed 2010 ftnerc https://doi.org/10.1016/j.jmarsys.2010.06.007 2023-02-04T19:35:45Z Arctic fresh water plays a large role in both the global ocean circulation and the hydrological cycle. To identify sources and pathways of the Arctic outflow into the North Atlantic, results of a high resolution global model and observations have been examined. It is shown that continental runoff and snowmelt are the dominant sources of Arctic fresh water. The simulations demonstrated that the oceanic transports account for the majority of the fresh water export from the Arctic into the North Atlantic. The oceanic outflow from the Arctic is split between the western route through the Canadian Arctic Archipelago and the eastern route through the Nordic Seas. Two thirds of total oceanic fresh water comes via the western route. Arctic halocline waters are present on both the western and eastern routes with the western route providing most of the Arctic upper halocline water. Sea ice export contributes more than half the total freshwater flux east of Greenland and less than one fifth of the freshwater flux west of it. Pacific water constitutes about third of the outflow of the Arctic upper halocline water into the North Atlantic. Article in Journal/Newspaper Arctic Arctic Archipelago Arctic Arctic Ocean Canadian Arctic Archipelago Greenland Nordic Seas North Atlantic Sea ice Natural Environment Research Council: NERC Open Research Archive Arctic Arctic Ocean Canadian Arctic Archipelago Greenland Pacific Journal of Marine Systems 83 1-2 14 37
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description Arctic fresh water plays a large role in both the global ocean circulation and the hydrological cycle. To identify sources and pathways of the Arctic outflow into the North Atlantic, results of a high resolution global model and observations have been examined. It is shown that continental runoff and snowmelt are the dominant sources of Arctic fresh water. The simulations demonstrated that the oceanic transports account for the majority of the fresh water export from the Arctic into the North Atlantic. The oceanic outflow from the Arctic is split between the western route through the Canadian Arctic Archipelago and the eastern route through the Nordic Seas. Two thirds of total oceanic fresh water comes via the western route. Arctic halocline waters are present on both the western and eastern routes with the western route providing most of the Arctic upper halocline water. Sea ice export contributes more than half the total freshwater flux east of Greenland and less than one fifth of the freshwater flux west of it. Pacific water constitutes about third of the outflow of the Arctic upper halocline water into the North Atlantic.
format Article in Journal/Newspaper
author Aksenov, Yevgeny
Bacon, Sheldon
Coward, Andrew C.
Holliday, N. Penny
spellingShingle Aksenov, Yevgeny
Bacon, Sheldon
Coward, Andrew C.
Holliday, N. Penny
Polar outflow from the Arctic Ocean: A high resolution model study
author_facet Aksenov, Yevgeny
Bacon, Sheldon
Coward, Andrew C.
Holliday, N. Penny
author_sort Aksenov, Yevgeny
title Polar outflow from the Arctic Ocean: A high resolution model study
title_short Polar outflow from the Arctic Ocean: A high resolution model study
title_full Polar outflow from the Arctic Ocean: A high resolution model study
title_fullStr Polar outflow from the Arctic Ocean: A high resolution model study
title_full_unstemmed Polar outflow from the Arctic Ocean: A high resolution model study
title_sort polar outflow from the arctic ocean: a high resolution model study
publishDate 2010
url http://nora.nerc.ac.uk/id/eprint/264033/
https://doi.org/10.1016/j.jmarsys.2010.06.007
geographic Arctic
Arctic Ocean
Canadian Arctic Archipelago
Greenland
Pacific
geographic_facet Arctic
Arctic Ocean
Canadian Arctic Archipelago
Greenland
Pacific
genre Arctic
Arctic Archipelago
Arctic
Arctic Ocean
Canadian Arctic Archipelago
Greenland
Nordic Seas
North Atlantic
Sea ice
genre_facet Arctic
Arctic Archipelago
Arctic
Arctic Ocean
Canadian Arctic Archipelago
Greenland
Nordic Seas
North Atlantic
Sea ice
op_relation Aksenov, Yevgeny orcid:0000-0001-6132-3434
Bacon, Sheldon orcid:0000-0002-2471-9373
Coward, Andrew C. orcid:0000-0002-9111-7700
Holliday, N. Penny orcid:0000-0002-9733-8002 . 2010 Polar outflow from the Arctic Ocean: A high resolution model study. Journal of Marine Systems, 83 (1-2). 14-37. https://doi.org/10.1016/j.jmarsys.2010.06.007 <https://doi.org/10.1016/j.jmarsys.2010.06.007>
op_doi https://doi.org/10.1016/j.jmarsys.2010.06.007
container_title Journal of Marine Systems
container_volume 83
container_issue 1-2
container_start_page 14
op_container_end_page 37
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