Seasoar CTD data for the SPURS-1 N. Atlantic field campaign(SPURS1_SEASOAR)
|Start/Stop Date||2013-Mar-22 to 2013-Apr-08|
|Description||The SPURS (Salinity Processes in the Upper Ocean Regional Study) project is an oceanographic process study and associated field program that aim to elucidate key mechanisms responsible for near-surface salinity variations in the oceans. The project involves two field campaigns and a series of cruises in regions of the Atlantic and Pacific Oceans exhibiting salinity extremes. SPURS employs a suite of state-of-the-art in-situ sampling technologies that, combined with remotely sensed salinity fields from the Aquarius/SAC-D and SMOS satellites, provide a detailed characterization of salinity structure over a continuum of spatio-temporal scales. The SPURS-1 campaign involved a series of 5 cruises during 2012 - 2013 seeking to characterize the salinity structure and balance in a high salinity, high evaporation, and low rainfall region of the subtropical North Atlantic. It aims to resolve processes responsible for maintaining the subtropical surface salinity maximum in this region and within a 900 x 800-mile square study area centered at 25N, 38W. The Seasoar is a towed vehicle equipped with impeller-forced wings that can be rotated on command to allow the vehicle to undulate in the upper ocean. Generally, Seasoar operates between the surface and about 400 meters depth while being towed on faired cable at about eight knots. A typical dive cycle takes about 12 minutes to complete, providing an up and down profile every 3 km. For SPURS-1, a Seasoar was deployed exclusively during the Sarmiento cruise over the period 22 Mar-8 Apr, 2013 and to a maximum depth of 312m. The Seasoar towed sensor system was equipped with dual pumped temperature/conductivity sensors. The Seasoar data in netCDF form here contains a highly processed 1-meter gridded version of the original source dataset, which is comprised of temperature, conductivity, salinity, pressure observations from 1144 casts during 2013 Spring SPURS Cruise.|
|Measurement||OCEANS > OCEAN TEMPERATURE > TEMPERATURE PROFILES|
OCEANS > SALINITY/DENSITY > CONDUCTIVITY
OCEANS > SALINITY/DENSITY > SALINITY
Name: ICM-CSIC Barcelona Sarmento SeaSoar (Seasoar)
Orbit Period: 0.0 minutes
Inclination Angle: 0.0 degrees
Name: Conductivity, Temperature, Depth (CTD)
Swath Width: 0.001 kilometers
Description: Spacecraft angular distance from orbital plane relative to the Equator.
|Project||NASA Salinity Processes in the Upper Ocean Regional Study (SPURS)|
|Data Provider||Publisher: SPURS Data Management PI, Fred Bingham|
Creator: SPURS PROJECT, Fred Bingham
Release Place: Department of Physics and Physical Oceanography, University on North Carolina, Wilmington, NC, USA
Release Date: 2015-May-11
|Keyword(s)||Seasoar, CTD, trajectory profile, Salinity, Conductivity, Temperature, Depth, Pressure, Upper Ocean, SPURS1, North Atlantic Ocean, salinity maximum region, insitu, SPURS, Sarmiento, ICM-CSIC Barcelona|
Questions related to this dataset? Contact firstname.lastname@example.org
Spatial Resolution: 1 Meters x 1 Meters
Temporal Resolution: 1 Day
Region: SPURS-1 N.Atlantic Salinity maximum region
North Bounding Coordinate: 26 degrees
South Bounding Coordinate: 22 degrees
West Bounding Coordinate: -39 degrees
East Bounding Coordinate: -36 degrees
Time Span: 2013-Mar-22 to 2013-Apr-08
Granule Time Span: 2013-Mar-22 to 2013-Apr-08
Ellipsoid: WGS 84
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|Available for access in-region with AWS Cloud|
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|DATA CITATION POLICY|
Citation is critically important for dataset documentation and discovery. Please cite the data as follows, and cite the reference papers when it is appropriate.
|Citation||SPURS PROJECT, Fred Bingham. 2015. SPURS Field Campaign Seasoar Products. Ver. 1.0. PO.DAAC, CA, USA. Dataset accessed [YYYY-MM-DD] at https://doi.org/10.5067/SPUR1-SEASR
For more information see Data Citations and Acknowledgments.
|Journal Reference||E.Lindstrom, F.Bryan, R.Schmitt. 2015. SPURS: Salinity Processes in the Upper-ocean Regional Study - The North Atlantic Experiment. Oceanography 28(1):14-19, http://dx.doi.org/10.5670/oceanog.2015.01.