Surface Salinity Variability in the North Atlantic During Recent Decades
The sea surface salinity (SSS) variability in the North Atlantic is investigated using numerical model simulations for the last 50 years based on atmospheric forcing variability from Comprehensive Atmosphere Ocean Data Set (COADS) and National Center for Environmental Prediction / National Center fo...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20010037382 2023-05-15T17:06:07+02:00 Surface Salinity Variability in the North Atlantic During Recent Decades Haekkinen, Sirpa Unclassified, Unlimited, Publicly available January 2001 application/pdf http://hdl.handle.net/2060/20010037382 unknown Document ID: 20010037382 http://hdl.handle.net/2060/20010037382 No Copyright CASI Oceanography 2001 ftnasantrs 2015-03-15T02:33:23Z The sea surface salinity (SSS) variability in the North Atlantic is investigated using numerical model simulations for the last 50 years based on atmospheric forcing variability from Comprehensive Atmosphere Ocean Data Set (COADS) and National Center for Environmental Prediction / National Center for Atmospheric Research (NCEP/NCAR) Reanalysis. The largest interannual and longer term variability occurs in two regions: the Labrador Sea and the North Equatorial Countercurrent (NECC) region. In both regions the seasonality of the surface salinity variability is prominent with the maximum standard deviation occurring in the summer/fall period. In the Labrador Sea the summer SSS anomalies far exceed those of wintertime in amplitude. The interannual SSS variability in the subpolar gyre can be attributed to two factors: excess ice melt and heat flux (i.e. deep mixing) variations. On the other hand, heat flux variability can also lead to meridional overturning changes on decadal time scales such that weak overturning is manifested in fresh surface conditions in the subpolar gyre. The overturning changes also influence the NECC region SSS variability. Moreover, the subpolar freshening events are expected to occur during the negative phase of North Atlantic Oscillation which is associated with a weak wintertime surface heat loss in the subpolar gyre. No excess sea ice melt or precipitation is necessary for the formation of the fresh anomalies, because with the lack of wide-spread deep mixing, the fresh water that would be expected based on climatology, would accumulate at the surface. Thus, the fresh water 'conveyor' in the Atlantic operates via the overturning circulation such that deep mixing inserts fresh water while removing heat from the water column. Other/Unknown Material Labrador Sea North Atlantic North Atlantic oscillation Sea ice NASA Technical Reports Server (NTRS) |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
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topic |
Oceanography |
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Oceanography Haekkinen, Sirpa Surface Salinity Variability in the North Atlantic During Recent Decades |
topic_facet |
Oceanography |
description |
The sea surface salinity (SSS) variability in the North Atlantic is investigated using numerical model simulations for the last 50 years based on atmospheric forcing variability from Comprehensive Atmosphere Ocean Data Set (COADS) and National Center for Environmental Prediction / National Center for Atmospheric Research (NCEP/NCAR) Reanalysis. The largest interannual and longer term variability occurs in two regions: the Labrador Sea and the North Equatorial Countercurrent (NECC) region. In both regions the seasonality of the surface salinity variability is prominent with the maximum standard deviation occurring in the summer/fall period. In the Labrador Sea the summer SSS anomalies far exceed those of wintertime in amplitude. The interannual SSS variability in the subpolar gyre can be attributed to two factors: excess ice melt and heat flux (i.e. deep mixing) variations. On the other hand, heat flux variability can also lead to meridional overturning changes on decadal time scales such that weak overturning is manifested in fresh surface conditions in the subpolar gyre. The overturning changes also influence the NECC region SSS variability. Moreover, the subpolar freshening events are expected to occur during the negative phase of North Atlantic Oscillation which is associated with a weak wintertime surface heat loss in the subpolar gyre. No excess sea ice melt or precipitation is necessary for the formation of the fresh anomalies, because with the lack of wide-spread deep mixing, the fresh water that would be expected based on climatology, would accumulate at the surface. Thus, the fresh water 'conveyor' in the Atlantic operates via the overturning circulation such that deep mixing inserts fresh water while removing heat from the water column. |
author |
Haekkinen, Sirpa |
author_facet |
Haekkinen, Sirpa |
author_sort |
Haekkinen, Sirpa |
title |
Surface Salinity Variability in the North Atlantic During Recent Decades |
title_short |
Surface Salinity Variability in the North Atlantic During Recent Decades |
title_full |
Surface Salinity Variability in the North Atlantic During Recent Decades |
title_fullStr |
Surface Salinity Variability in the North Atlantic During Recent Decades |
title_full_unstemmed |
Surface Salinity Variability in the North Atlantic During Recent Decades |
title_sort |
surface salinity variability in the north atlantic during recent decades |
publishDate |
2001 |
url |
http://hdl.handle.net/2060/20010037382 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Labrador Sea North Atlantic North Atlantic oscillation Sea ice |
genre_facet |
Labrador Sea North Atlantic North Atlantic oscillation Sea ice |
op_source |
CASI |
op_relation |
Document ID: 20010037382 http://hdl.handle.net/2060/20010037382 |
op_rights |
No Copyright |
_version_ |
1766061111744921600 |