The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography
The number of direct observations of ocean currents in the central Arctic are still limited. Here, the Arctic Ocean Circulation is studied using available altimetric, bathymetric and hydrographic data sets. Based on earlier theoretical frameworks of the Arctic Ocean Circulation, such as Nøst and Isa...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5021543 2023-07-30T04:00:23+02:00 The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography Kallmyr, J. Nilsson, J. Isachsen, P. Sjur, A. Chafik, L. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021543 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4104 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021543 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-4104 2023-07-09T23:40:20Z The number of direct observations of ocean currents in the central Arctic are still limited. Here, the Arctic Ocean Circulation is studied using available altimetric, bathymetric and hydrographic data sets. Based on earlier theoretical frameworks of the Arctic Ocean Circulation, such as Nøst and Isachsen (2003), key concepts such as topographic steering of the flow field, and the degree to which it is eqvivalently barotropic are evaluated. It is found that the surface flow, which is derived from altimetry, is generally aligned along large-scale depth contours. A closer study of central regions in the Arctic Mediterranean also show high alignment along local depth contours in both the Nordic Seas and the Arctic Ocean. While the bottom flow is estimated through thermal wind balance, and as such have a lower horizontal resolution, many of the same features are seen, suggesting that the circulation is generally eqvivalent barotropic. Local regions of cross-slope flow are identified as areas of inflow (outflow) to (from) the Arctic Ocean, suggesting that the local relative vorticity is enough to break topographic steering in these regions. Addtionally, different hydrographic data sets yield slightly different thermal wind velocities, but which can affect the direction and magnitude of the bottom flow. Conference Object Arctic Arctic Ocean Nordic Seas GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic Arctic Ocean Isachsen ENVELOPE(-103.505,-103.505,78.785,78.785) |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
The number of direct observations of ocean currents in the central Arctic are still limited. Here, the Arctic Ocean Circulation is studied using available altimetric, bathymetric and hydrographic data sets. Based on earlier theoretical frameworks of the Arctic Ocean Circulation, such as Nøst and Isachsen (2003), key concepts such as topographic steering of the flow field, and the degree to which it is eqvivalently barotropic are evaluated. It is found that the surface flow, which is derived from altimetry, is generally aligned along large-scale depth contours. A closer study of central regions in the Arctic Mediterranean also show high alignment along local depth contours in both the Nordic Seas and the Arctic Ocean. While the bottom flow is estimated through thermal wind balance, and as such have a lower horizontal resolution, many of the same features are seen, suggesting that the circulation is generally eqvivalent barotropic. Local regions of cross-slope flow are identified as areas of inflow (outflow) to (from) the Arctic Ocean, suggesting that the local relative vorticity is enough to break topographic steering in these regions. Addtionally, different hydrographic data sets yield slightly different thermal wind velocities, but which can affect the direction and magnitude of the bottom flow. |
format |
Conference Object |
author |
Kallmyr, J. Nilsson, J. Isachsen, P. Sjur, A. Chafik, L. |
spellingShingle |
Kallmyr, J. Nilsson, J. Isachsen, P. Sjur, A. Chafik, L. The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography |
author_facet |
Kallmyr, J. Nilsson, J. Isachsen, P. Sjur, A. Chafik, L. |
author_sort |
Kallmyr, J. |
title |
The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography |
title_short |
The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography |
title_full |
The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography |
title_fullStr |
The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography |
title_full_unstemmed |
The Arctic Ocean surface and bottom circulation estimated from altimetry and hydrography |
title_sort |
arctic ocean surface and bottom circulation estimated from altimetry and hydrography |
publishDate |
2023 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021543 |
long_lat |
ENVELOPE(-103.505,-103.505,78.785,78.785) |
geographic |
Arctic Arctic Ocean Isachsen |
geographic_facet |
Arctic Arctic Ocean Isachsen |
genre |
Arctic Arctic Ocean Nordic Seas |
genre_facet |
Arctic Arctic Ocean Nordic Seas |
op_source |
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-4104 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021543 |
op_doi |
https://doi.org/10.57757/IUGG23-4104 |
_version_ |
1772810878742167552 |