SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment
In this special issue of Oceanography, we explore the results of SPURS-1, the first part of the ocean process study Salinity Processes in the Upper-ocean Regional Study (SPURS). The experiment was conducted between August 2012 and October 2013 in the subtropical North Atlantic and was the first of t...
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Online Access: | http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-781 https://doi.org/10.5670/oceanog.2015.01 |
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ftncar:oai:drupal-site.org:articles_16708 2023-09-05T13:21:27+02:00 SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment Lindstrom, Eric (author) Bryan, Frank (author) Schmitt, Ray (author) 2015-03-01 http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-781 https://doi.org/10.5670/oceanog.2015.01 en eng Oceanography http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-781 doi:10.5670/oceanog.2015.01 ark:/85065/d7qv3np7 Copyright 2015 Oceanography Society. Text article 2015 ftncar https://doi.org/10.5670/oceanog.2015.01 2023-08-14T18:45:03Z In this special issue of Oceanography, we explore the results of SPURS-1, the first part of the ocean process study Salinity Processes in the Upper-ocean Regional Study (SPURS). The experiment was conducted between August 2012 and October 2013 in the subtropical North Atlantic and was the first of two experiments (SPURS come in pairs!). SPURS-2 is planned for 2016-2017 in the tropical eastern Pacific Ocean. The scientific motivation behind SPURS arises from the desire to understand the patterns and variations of salinity at the ocean’s surface. To first order, surface salinity patterns reflect the overlying patterns of evaporation and precipitation that force the freshwater balance in the upper ocean (Wüst, 1936). Maps of the net difference between evaporation and precipitation (E-P) appear to be quite similar in pattern to surface salinity. If the surface salinity is determined only by (E-P), then the ocean itself might serve as crude "rain gauge." In fact, it is already known that ocean circulation in the form of wind-driven surface currents must be accounted for in understanding surface salinity patterns (surface salinity maxima are offset poleward of subtropical E-P maxima due to Ekman currents induced by the trade winds). In addition, ocean mixing processes also affect the temporal evolution of surface salinity. SPURS was designed to examine the salinity balance in the upper ocean through observation of salinity and ocean circulation on a variety of scales. Article in Journal/Newspaper North Atlantic OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Pacific Wüst ENVELOPE(-60.843,-60.843,-72.346,-72.346) Oceanography 28 1 14 19 |
institution |
Open Polar |
collection |
OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) |
op_collection_id |
ftncar |
language |
English |
description |
In this special issue of Oceanography, we explore the results of SPURS-1, the first part of the ocean process study Salinity Processes in the Upper-ocean Regional Study (SPURS). The experiment was conducted between August 2012 and October 2013 in the subtropical North Atlantic and was the first of two experiments (SPURS come in pairs!). SPURS-2 is planned for 2016-2017 in the tropical eastern Pacific Ocean. The scientific motivation behind SPURS arises from the desire to understand the patterns and variations of salinity at the ocean’s surface. To first order, surface salinity patterns reflect the overlying patterns of evaporation and precipitation that force the freshwater balance in the upper ocean (Wüst, 1936). Maps of the net difference between evaporation and precipitation (E-P) appear to be quite similar in pattern to surface salinity. If the surface salinity is determined only by (E-P), then the ocean itself might serve as crude "rain gauge." In fact, it is already known that ocean circulation in the form of wind-driven surface currents must be accounted for in understanding surface salinity patterns (surface salinity maxima are offset poleward of subtropical E-P maxima due to Ekman currents induced by the trade winds). In addition, ocean mixing processes also affect the temporal evolution of surface salinity. SPURS was designed to examine the salinity balance in the upper ocean through observation of salinity and ocean circulation on a variety of scales. |
author2 |
Lindstrom, Eric (author) Bryan, Frank (author) Schmitt, Ray (author) |
format |
Article in Journal/Newspaper |
title |
SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment |
spellingShingle |
SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment |
title_short |
SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment |
title_full |
SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment |
title_fullStr |
SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment |
title_full_unstemmed |
SPURS: Salinity processes in the upper-ocean regional study-- The North Atlantic experiment |
title_sort |
spurs: salinity processes in the upper-ocean regional study-- the north atlantic experiment |
publishDate |
2015 |
url |
http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-781 https://doi.org/10.5670/oceanog.2015.01 |
long_lat |
ENVELOPE(-60.843,-60.843,-72.346,-72.346) |
geographic |
Pacific Wüst |
geographic_facet |
Pacific Wüst |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Oceanography http://nldr.library.ucar.edu/repository/collections/OSGC-000-000-021-781 doi:10.5670/oceanog.2015.01 ark:/85065/d7qv3np7 |
op_rights |
Copyright 2015 Oceanography Society. |
op_doi |
https://doi.org/10.5670/oceanog.2015.01 |
container_title |
Oceanography |
container_volume |
28 |
container_issue |
1 |
container_start_page |
14 |
op_container_end_page |
19 |
_version_ |
1776202059872206848 |