Heat and freshwater fluxes through the Nordic seas

The major exchanges of volume, heat, and freshwater between the Arctic Ocean and the World Ocean occur through the Nordic seas. Here is presented the northernmost estimate for the oceanic transport of these properties that is derived from a set of hydrographic and direct current measurements, using...

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Main Authors: Oliver, Kevin I.C., Heywood, Karen J.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2003
Subjects:
Online Access:https://eprints.soton.ac.uk/68795/
http://ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F1520-0485(2003)033%3C1009:HAFFTT%3E2.0.CO%3B2&ct=1
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spelling ftsouthampton:oai:eprints.soton.ac.uk:68795 2023-07-30T04:01:18+02:00 Heat and freshwater fluxes through the Nordic seas Oliver, Kevin I.C. Heywood, Karen J. 2003-05 https://eprints.soton.ac.uk/68795/ http://ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F1520-0485(2003)033%3C1009:HAFFTT%3E2.0.CO%3B2&ct=1 unknown Oliver, Kevin I.C. and Heywood, Karen J. (2003) Heat and freshwater fluxes through the Nordic seas. Journal of Physical Oceanography, 33 (5), 1009-1026. (doi:10.1175/1520-0485(2003)033<1009:HAFFTT>2.0.CO;2 <http://dx.doi.org/10.1175/1520-0485(2003)033<1009:HAFFTT>2.0.CO;2>). Article PeerReviewed 2003 ftsouthampton https://doi.org/10.1175/1520-0485(2003)033<1009:HAFFTT>2.0.CO;2 2023-07-09T21:06:17Z The major exchanges of volume, heat, and freshwater between the Arctic Ocean and the World Ocean occur through the Nordic seas. Here is presented the northernmost estimate for the oceanic transport of these properties that is derived from a set of hydrographic and direct current measurements, using a lowered acoustic Doppler current profiler, between the Greenland and European coasts. By applying box inverse methods to a synoptic section from the summer of 1999, a heat transport of 0.20+/-0.08 PW toward the Arctic and a freshwater transport of 0.10+/-0.05 Sv (1 Svequivalent to10(6) m(3) s(-1)) away from the Arctic are calculated, with a likely additional freshwater transport on the order of 0.05 Sv near the Greenland coast. Uncertainties associated with how representative the section is of the seasonal mean are included in the error analysis. Large depth-independent components in the currents throughout the section, including the Atlantic inflow, are observed. The increase (decrease) in the heat transport resulting from an increase (decrease) in the transport of this inflow is 0.033 PW Sv(-1), and this is the dominant source of uncertainty in the solution. Therefore, determining only depth-dependent transports is unlikely to be sufficient when measuring heat transport in the region. The overturning components of the section heat and freshwater transport are 0.15+/-0.07 PW and 0.04+/-0.02 Sv, respectively. From the horizontal transport of layers within the section, a densification of 4.3+/-2.5 Sv of waters north of the section is predicted, to densities greater than the boundary between inflow and outflow waters between the Atlantic Ocean and the Nordic seas. Article in Journal/Newspaper Arctic Arctic Ocean Greenland Nordic Seas University of Southampton: e-Prints Soton Arctic Arctic Ocean Greenland
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language unknown
description The major exchanges of volume, heat, and freshwater between the Arctic Ocean and the World Ocean occur through the Nordic seas. Here is presented the northernmost estimate for the oceanic transport of these properties that is derived from a set of hydrographic and direct current measurements, using a lowered acoustic Doppler current profiler, between the Greenland and European coasts. By applying box inverse methods to a synoptic section from the summer of 1999, a heat transport of 0.20+/-0.08 PW toward the Arctic and a freshwater transport of 0.10+/-0.05 Sv (1 Svequivalent to10(6) m(3) s(-1)) away from the Arctic are calculated, with a likely additional freshwater transport on the order of 0.05 Sv near the Greenland coast. Uncertainties associated with how representative the section is of the seasonal mean are included in the error analysis. Large depth-independent components in the currents throughout the section, including the Atlantic inflow, are observed. The increase (decrease) in the heat transport resulting from an increase (decrease) in the transport of this inflow is 0.033 PW Sv(-1), and this is the dominant source of uncertainty in the solution. Therefore, determining only depth-dependent transports is unlikely to be sufficient when measuring heat transport in the region. The overturning components of the section heat and freshwater transport are 0.15+/-0.07 PW and 0.04+/-0.02 Sv, respectively. From the horizontal transport of layers within the section, a densification of 4.3+/-2.5 Sv of waters north of the section is predicted, to densities greater than the boundary between inflow and outflow waters between the Atlantic Ocean and the Nordic seas.
format Article in Journal/Newspaper
author Oliver, Kevin I.C.
Heywood, Karen J.
spellingShingle Oliver, Kevin I.C.
Heywood, Karen J.
Heat and freshwater fluxes through the Nordic seas
author_facet Oliver, Kevin I.C.
Heywood, Karen J.
author_sort Oliver, Kevin I.C.
title Heat and freshwater fluxes through the Nordic seas
title_short Heat and freshwater fluxes through the Nordic seas
title_full Heat and freshwater fluxes through the Nordic seas
title_fullStr Heat and freshwater fluxes through the Nordic seas
title_full_unstemmed Heat and freshwater fluxes through the Nordic seas
title_sort heat and freshwater fluxes through the nordic seas
publishDate 2003
url https://eprints.soton.ac.uk/68795/
http://ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F1520-0485(2003)033%3C1009:HAFFTT%3E2.0.CO%3B2&ct=1
geographic Arctic
Arctic Ocean
Greenland
geographic_facet Arctic
Arctic Ocean
Greenland
genre Arctic
Arctic Ocean
Greenland
Nordic Seas
genre_facet Arctic
Arctic Ocean
Greenland
Nordic Seas
op_relation Oliver, Kevin I.C. and Heywood, Karen J. (2003) Heat and freshwater fluxes through the Nordic seas. Journal of Physical Oceanography, 33 (5), 1009-1026. (doi:10.1175/1520-0485(2003)033<1009:HAFFTT>2.0.CO;2 <http://dx.doi.org/10.1175/1520-0485(2003)033<1009:HAFFTT>2.0.CO;2>).
op_doi https://doi.org/10.1175/1520-0485(2003)033<1009:HAFFTT>2.0.CO;2
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