Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations
Author Posting. © American Meteorological Society, 2020. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 50(11), (2020): 3235–3251, https://doi.org/10.1175/...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/27490 2023-05-15T15:15:21+02:00 Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations Lin, Peigen Pickart, Robert S. Jochumsen, Kerstin Moore, G. W. K. Valdimarsson, Héðinn Fristedt, Tim Pratt, Lawrence J. 2020-11-01 https://hdl.handle.net/1912/27490 unknown American Meteorological Society https://doi.org/10.1175/JPO-D-20-0095.1 Lin, P., Pickart, R. S., Jochumsen, K., Moore, G. W. K., Valdimarsson, H., Fristedt, T., & Pratt, L. J. (2020). Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations. Journal of Physical Oceanography, 50(11), 3235–3251. https://hdl.handle.net/1912/27490 doi:10.1175/JPO-D-20-0095.1 Lin, P., Pickart, R. S., Jochumsen, K., Moore, G. W. K., Valdimarsson, H., Fristedt, T., & Pratt, L. J. (2020). Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations. Journal of Physical Oceanography, 50(11), 3235–3251. doi:10.1175/JPO-D-20-0095.1 Currents Instability Ocean circulation Ocean dynamics Potential vorticity Article 2020 ftwhoas https://doi.org/10.1175/JPO-D-20-0095.1 2022-05-28T23:04:15Z Author Posting. © American Meteorological Society, 2020. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 50(11), (2020): 3235–3251, https://doi.org/10.1175/JPO-D-20-0095.1. The dense outflow through Denmark Strait is the largest contributor to the lower limb of the Atlantic meridional overturning circulation, yet a description of the full velocity field across the strait remains incomplete. Here we analyze a set of 22 shipboard hydrographic–velocity sections occupied along the Látrabjarg transect at the Denmark Strait sill, obtained over the time period 1993–2018. The sections provide the first complete view of the kinematic components at the sill: the shelfbreak East Greenland Current (EGC), the combined flow of the separated EGC, and the North Icelandic Jet (NIJ), and the northward-flowing North Icelandic Irminger Current (NIIC). The total mean transport of overflow water is 3.54 ± 0.29 Sv (1 Sv ≡ 106 m3 s−1), comparable to previous estimates. The dense overflow is partitioned in terms of water mass constituents and flow components. The mean transports of the two types of overflow water—Atlantic-origin Overflow Water and Arctic-origin Overflow Water—are comparable in Denmark Strait, while the merged NIJ–separated EGC transports 55% more water than the shelfbreak EGC. A significant degree of water mass exchange takes place between the branches as they converge in Denmark Strait. There are two dominant time-varying configurations of the flow that are characterized as a cyclonic state and a noncyclonic state. These appear to be wind-driven. A potential vorticity analysis indicates that the flow through Denmark Strait is subject to symmetric instability. This occurs at the top of the overflow layer, implying that the mixing/entrainment process that modifies the overflow water begins at the sill. Funding for the study was provided by National Science Foundation (NSF) ... Article in Journal/Newspaper Arctic Denmark Strait East Greenland east greenland current Greenland North Icelandic Irminger Current NIIC Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Arctic Greenland Látrabjarg ENVELOPE(-24.532,-24.532,65.503,65.503) Journal of Physical Oceanography 50 11 3235 3251 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
unknown |
topic |
Currents Instability Ocean circulation Ocean dynamics Potential vorticity |
spellingShingle |
Currents Instability Ocean circulation Ocean dynamics Potential vorticity Lin, Peigen Pickart, Robert S. Jochumsen, Kerstin Moore, G. W. K. Valdimarsson, Héðinn Fristedt, Tim Pratt, Lawrence J. Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations |
topic_facet |
Currents Instability Ocean circulation Ocean dynamics Potential vorticity |
description |
Author Posting. © American Meteorological Society, 2020. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 50(11), (2020): 3235–3251, https://doi.org/10.1175/JPO-D-20-0095.1. The dense outflow through Denmark Strait is the largest contributor to the lower limb of the Atlantic meridional overturning circulation, yet a description of the full velocity field across the strait remains incomplete. Here we analyze a set of 22 shipboard hydrographic–velocity sections occupied along the Látrabjarg transect at the Denmark Strait sill, obtained over the time period 1993–2018. The sections provide the first complete view of the kinematic components at the sill: the shelfbreak East Greenland Current (EGC), the combined flow of the separated EGC, and the North Icelandic Jet (NIJ), and the northward-flowing North Icelandic Irminger Current (NIIC). The total mean transport of overflow water is 3.54 ± 0.29 Sv (1 Sv ≡ 106 m3 s−1), comparable to previous estimates. The dense overflow is partitioned in terms of water mass constituents and flow components. The mean transports of the two types of overflow water—Atlantic-origin Overflow Water and Arctic-origin Overflow Water—are comparable in Denmark Strait, while the merged NIJ–separated EGC transports 55% more water than the shelfbreak EGC. A significant degree of water mass exchange takes place between the branches as they converge in Denmark Strait. There are two dominant time-varying configurations of the flow that are characterized as a cyclonic state and a noncyclonic state. These appear to be wind-driven. A potential vorticity analysis indicates that the flow through Denmark Strait is subject to symmetric instability. This occurs at the top of the overflow layer, implying that the mixing/entrainment process that modifies the overflow water begins at the sill. Funding for the study was provided by National Science Foundation (NSF) ... |
format |
Article in Journal/Newspaper |
author |
Lin, Peigen Pickart, Robert S. Jochumsen, Kerstin Moore, G. W. K. Valdimarsson, Héðinn Fristedt, Tim Pratt, Lawrence J. |
author_facet |
Lin, Peigen Pickart, Robert S. Jochumsen, Kerstin Moore, G. W. K. Valdimarsson, Héðinn Fristedt, Tim Pratt, Lawrence J. |
author_sort |
Lin, Peigen |
title |
Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations |
title_short |
Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations |
title_full |
Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations |
title_fullStr |
Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations |
title_full_unstemmed |
Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations |
title_sort |
kinematic structure and dynamics of the denmark strait overflow from ship-based observations |
publisher |
American Meteorological Society |
publishDate |
2020 |
url |
https://hdl.handle.net/1912/27490 |
long_lat |
ENVELOPE(-24.532,-24.532,65.503,65.503) |
geographic |
Arctic Greenland Látrabjarg |
geographic_facet |
Arctic Greenland Látrabjarg |
genre |
Arctic Denmark Strait East Greenland east greenland current Greenland North Icelandic Irminger Current NIIC |
genre_facet |
Arctic Denmark Strait East Greenland east greenland current Greenland North Icelandic Irminger Current NIIC |
op_source |
Lin, P., Pickart, R. S., Jochumsen, K., Moore, G. W. K., Valdimarsson, H., Fristedt, T., & Pratt, L. J. (2020). Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations. Journal of Physical Oceanography, 50(11), 3235–3251. doi:10.1175/JPO-D-20-0095.1 |
op_relation |
https://doi.org/10.1175/JPO-D-20-0095.1 Lin, P., Pickart, R. S., Jochumsen, K., Moore, G. W. K., Valdimarsson, H., Fristedt, T., & Pratt, L. J. (2020). Kinematic structure and dynamics of the Denmark Strait Overflow from ship-based observations. Journal of Physical Oceanography, 50(11), 3235–3251. https://hdl.handle.net/1912/27490 doi:10.1175/JPO-D-20-0095.1 |
op_doi |
https://doi.org/10.1175/JPO-D-20-0095.1 |
container_title |
Journal of Physical Oceanography |
container_volume |
50 |
container_issue |
11 |
container_start_page |
3235 |
op_container_end_page |
3251 |
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1766345724722675712 |