Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013

The overall goal of this study is to obtain a quantitative description of the water mass composition, kinematics, and dynamics of the Atlantic water boundary current in the eastern Arctic Ocean over an annual cycle, in order to elucidate the role of the current in regulating the Arctic system. The p...

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Main Author: McRaven, Leah
Format: Dataset
Language:English
Published: NSF Arctic Data Center 2018
Subjects:
Online Access:https://dx.doi.org/10.18739/a2tq5rf2n
https://arcticdata.io/catalog/view/doi:10.18739/A2TQ5RF2N
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record_format openpolar
spelling ftdatacite:10.18739/a2tq5rf2n 2023-05-15T14:52:38+02:00 Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013 McRaven, Leah 2018 text/xml https://dx.doi.org/10.18739/a2tq5rf2n https://arcticdata.io/catalog/view/doi:10.18739/A2TQ5RF2N en eng NSF Arctic Data Center Physical Oceanography Mooring Observations Atlantic Water Inflow Experiment ATWAIN A-TWAIN dataset Dataset 2018 ftdatacite https://doi.org/10.18739/a2tq5rf2n 2021-11-05T12:55:41Z The overall goal of this study is to obtain a quantitative description of the water mass composition, kinematics, and dynamics of the Atlantic water boundary current in the eastern Arctic Ocean over an annual cycle, in order to elucidate the role of the current in regulating the Arctic system. The project is part of a larger cooperative program entitled the Atlantic Water Inflow Experiment (ATWAIN), which is an international collaboration between six institutions: The Woods Hole Oceanographic Institution (WHOI), USA; the Institute for Marine Research in Bergen, Norway (IMR); the Norwegian Polar Institute (NPI); the University of Svalbard (UNIS); the University of Tromsø (UT); and the Institute of Oceanology Polish Academy of Sciences (IOPAS). The main goal of ATWAIN is to better understand how the Atlantic water spreads into the Arctic Ocean, including the manner in which it interacts with the pack-ice and how it is transformed within the Eurasian Basin. As part of our study, six moorings were deployed across the Atlantic water boundary current near 30E for a one-year period, from September 2012 to September 2013. WHOI provided the four offshore moorings in the array. Dataset Arctic Arctic Ocean Norwegian Polar Institute Svalbard UNIS University of Tromsø DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean Bergen Norway Svalbard Tromsø
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Physical Oceanography
Mooring Observations
Atlantic Water Inflow Experiment
ATWAIN
A-TWAIN
spellingShingle Physical Oceanography
Mooring Observations
Atlantic Water Inflow Experiment
ATWAIN
A-TWAIN
McRaven, Leah
Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013
topic_facet Physical Oceanography
Mooring Observations
Atlantic Water Inflow Experiment
ATWAIN
A-TWAIN
description The overall goal of this study is to obtain a quantitative description of the water mass composition, kinematics, and dynamics of the Atlantic water boundary current in the eastern Arctic Ocean over an annual cycle, in order to elucidate the role of the current in regulating the Arctic system. The project is part of a larger cooperative program entitled the Atlantic Water Inflow Experiment (ATWAIN), which is an international collaboration between six institutions: The Woods Hole Oceanographic Institution (WHOI), USA; the Institute for Marine Research in Bergen, Norway (IMR); the Norwegian Polar Institute (NPI); the University of Svalbard (UNIS); the University of Tromsø (UT); and the Institute of Oceanology Polish Academy of Sciences (IOPAS). The main goal of ATWAIN is to better understand how the Atlantic water spreads into the Arctic Ocean, including the manner in which it interacts with the pack-ice and how it is transformed within the Eurasian Basin. As part of our study, six moorings were deployed across the Atlantic water boundary current near 30E for a one-year period, from September 2012 to September 2013. WHOI provided the four offshore moorings in the array.
format Dataset
author McRaven, Leah
author_facet McRaven, Leah
author_sort McRaven, Leah
title Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013
title_short Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013
title_full Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013
title_fullStr Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013
title_full_unstemmed Mooring Observations from the Atlantic Water Inflow Experiment (ATWAIN) for mooring EA4 at 81.88882°N and 30.09648°E from September 21, 2012 through September 19, 2013
title_sort mooring observations from the atlantic water inflow experiment (atwain) for mooring ea4 at 81.88882°n and 30.09648°e from september 21, 2012 through september 19, 2013
publisher NSF Arctic Data Center
publishDate 2018
url https://dx.doi.org/10.18739/a2tq5rf2n
https://arcticdata.io/catalog/view/doi:10.18739/A2TQ5RF2N
geographic Arctic
Arctic Ocean
Bergen
Norway
Svalbard
Tromsø
geographic_facet Arctic
Arctic Ocean
Bergen
Norway
Svalbard
Tromsø
genre Arctic
Arctic Ocean
Norwegian Polar Institute
Svalbard
UNIS
University of Tromsø
genre_facet Arctic
Arctic Ocean
Norwegian Polar Institute
Svalbard
UNIS
University of Tromsø
op_doi https://doi.org/10.18739/a2tq5rf2n
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