RSS SMAP Level 2C Sea Surface Salinity NRT V6.0 Validated Dataset

(SMAP_RSS_L2_SSS_NRT_V6)
Version6.0
Processing Level2
Start/Stop Date2022-Jul-28 to Present
Short NameSMAP_RSS_L2_SSS_NRT_V6
DescriptionThe SMAP-SSS level 2C near real-time (NRT) V6.0 dataset produced by the Remote Sensing Systems (RSS) and sponsored by the NASA Ocean Salinity Science Team, is a validated product that provides near real-time orbital/swath data on sea surface salinity (SSS) derived from the NASA's Soil Moisture Active Passive (SMAP) mission. SMAP, launched on January 31, 2015, was initially designed to measure and map Earth's soil moisture and freeze/thaw state to better understand terrestrial water, carbon and energy cycles, and has been adapted to measure ocean SSS and ocean wind speed using its passive microwave instrument. The SMAP instrument is in a near polar orbiting, sun synchronous orbit with a nominal 8 day repeat cycle.

The dataset includes derived SMAP SSS, SSS uncertainty using the NRT SMAP Salinity Retrieval Algorithm, top of atmosphere brightness temperature (TB), wind speed and direction data for extreme winds, and other all necessary ancillary data and the results of all intermediate steps. The observations are global, provided on a 0.25° fixed Earth grid with an approximate spatial resolution of 70 km. The major changes in Version 6.0 from Version 5.0 are: (1) Removal of biases during the first few months of the SMAP mission that are related to the operation of the SMAP radar during that time. (2) Mitigation of biases that depend on the SMAP look angle. (3) Mitigation of salty biases at high Northern latitudes. (4) Revised sun-glint flag. Each data file covers one 98-minute orbit (15 files per day), is available in netCDF-4 file format with about 5 hours l atency.

This RSS SMAP-SSS V6.0 NRT dataset holds tremendous potential for scientific research and various applications. Given the SMAP satellite's near-polar orbit and sun-synchronous nature with its 1000km swath, it achieves global coverage in approximately three days, enabling researchers to monitor and model global oceanic and climatic phenomena with unprecedented detail and timeliness. These data can inform and enhance understanding of global weather patterns, the Earth’s hydrological cycle, ocean circulation, and climate change.
DOI10.5067/SMP60-2SNRT
MeasurementOCEANS > SALINITY/DENSITY > SALINITY
Swath Width1000 km
Platform/Sensor
SMAP
Platform
Name: Soil Moisture Active and Passive Observatory (SMAP)
Orbit Period: 98.5 minutes
Inclination Angle: 98.0 degrees
/
SMAP L-BAND RADIOMETER
SENSOR
Name: SMAP L-Band Radiometer (SMAP L-BAND RADIOMETER)
Swath Width: 1000.0 kilometers
Description: Spacecraft angular distance from orbital plane relative to the Equator.

ProjectSoil Moisture Active Passive (SMAP)
Data ProviderPublisher: Remote Sensing Systems (RSS)
Creator: Remote Sensing Systems (RSS)
Release Place: Remote Sensing Systems, 444 Tenth Street, Suite 200, Santa Rosa, CA 95401, USA
Release Date: 2024-Mar-26
Resource: http://podaac.jpl.nasa.gov/smap

FormatnetCDF-4
Keyword(s)RssSmapSSSv6, V6, SMAP, SMAP-SSS, Soil Moisture Active Passive, salinity, polar, sun-synchronous, sss, psu, NASA, project, mission, RSS, Remote Sensing System, REMSS, NRT, near real-time
Questions related to this dataset? Contact podaac@podaac.jpl.nasa.gov
Resolution
Spatial Resolution: 0.25 Decimal Degrees x 0.25 Decimal Degrees
Temporal Resolution: Hourly - < Daily
 
Coverage
Region: GLOBAL
North Bounding Coordinate: 90 degrees
South Bounding Coordinate: -90 degrees
West Bounding Coordinate: -180 degrees
East Bounding Coordinate: 180 degrees
Time Span: 2022-Jul-28 to Present
Swath Width: 1000 km
 
Projection
Projection Type: Grid
 
NameLong NameUnit
alphaScan angle: +90 is left of forward. +270 is right of forward.degree
anc_sea_ice_flagancillary sea-ice detection indicator1
cellatLatitude of OI Earth grid celldegrees_north
cellonLongitude of OI Earth grid celldegrees_east
dtb_land_correctionTA land correction applied at TOA. Pol basis V,HKelvin
dtemp_antEmpirical correction to physical temperature of reflector. Pol basis V,HKelvin
eaaAzimuthal look angle relative to Northdegree
eiaEarth incidence angledegree
flandland fraction within footprint1
gallatLatitudinal (polar) angle of specular reflection ray in ECI2000degree
gallonLongitudinal (azimuthal) angle of specular reflection ray in ECI2000degree
glandland fraction weighted by antenna gain1
iqc_flag32-bit quality control flag1
mongltMoon glint angledegree
praPolarization basis rotation angle (geometric part)degree
pratot_expExpected total polarization basis rotation angle: Faraday rotation (from external TEC) + geometricdegree
rainrain rate. estimated from NCEP could water profilesmm h-1
sea_ice_zonessea-ice contamination zones1
solar_fluxAncillary solar flux (from NOAA SWPC)1e-22 W m-2 Hz-1
sss_refReference sea surface salinity from HYCOM1e-3
sss_smapSMAP sea surface salinity smoothed to approx 70km resolution1e-3
sss_smap_40kmSMAP sea surface salinity at original 40km resolution1e-3
sss_smap_40km_unctotal formal uncertainty estimate of SMAP sea surface salinity at original 40km resolution1e-3
sss_smap_40km_unc_compformal uncertainty components of SMAP sea surface salinity at original 40km resolution1e-3
sss_smap_unctotal formal uncertainty estimate of SMAP sea surface salinity smoothed to approx 70km resolution1e-3
sss_smap_unc_compformal uncertainty components of SMAP sea surface salinity smoothed to approx 70km resolution1e-3
sun_alphaSun azimuth angle in S/C coordinate systemdegree
sun_betaSun zenith angle in S/C coordinate systemdegree
sungltSun glint angle. Negative value means that sun ray pierces the Earth.degree
surtepAncillary sea surface temperature (from CMC)Kelvin
ta_antunfiltered antenna temperature. Pol basis V,H,S3,S4Kelvin
ta_ant_calibratedAntenna temperature after correcting for emissive reflector and TND adjustment. Pol basis V,H,S3,S4Kelvin
ta_ant_expExpected (RTM) antenna temperature before any losses. This is to be compared with ta_ant_calibrated. Pol basis V,H,S3,S4Kelvin
ta_ant_filteredRFI filtered antenna temperature. Pol basis V,H,S3,S4Kelvin
ta_earthAntenna temperature after correcting for cold space, galaxy, sun, moon. Pol basis V,H,S3,S4Kelvin
ta_gal_dirTA of direct galaxy intrusion. Pol basis I,Q,S3Kelvin
ta_gal_refTA of reflected galaxy intrusion. Pol basis I,Q,S3Kelvin
ta_sun_dirTA of direct sun intrusion. Pol basis I,Q,S3Kelvin
ta_sun_refTA of reflected sun intrusion. Pol basis I,Q,S3Kelvin
tb_consistencysqrt(chi2) of MLE in SSS retrievalKelvin
tb_surBrightness temperature at rough ocean surface BEFORE applying roughness correction. Pol basis V,H,S3,S4Kelvin
tb_sur0Brightness temperature at flat ocean surface AFTER applying roughness correction. Pol basis V,H,S3,S4Kelvin
tb_sur0_expExpected (RTM) at flat ocean surface. SIC added. This is to be compared with tb_sur0, before SIC. Pol basis V,H,S3,S4Kelvin
tb_sur0_sicBrightness temperature at flat ocean surface after applying roughness correction and sea-ice correction. Pol basis V,H,S3,S4Kelvin
tb_toaBrightness temperature at top of atmosphere BEFORE applying land correction. Pol basis V,H,S3,S4Kelvin
tb_toa_lcBrightness temperature at top of atmosphere AFTER applying land correction. Pol basis V,H,S3,S4Kelvin
tb_toiBrightness temperature at top of ionosphere. Pol basis V,H,S3,S4Kelvin
tbdwAtmospheric downwelling brightness temperatureKelvin
tbupAtmospheric upwelling brightness temperatureKelvin
TECVertically integrated electron content between surface and S/C1e16 m-2
temp_antPhysical temperature of reflector from L1B files. Pol basis V,HKelvin
timeTime of observationseconds since 2000-1-1 0:0:0 0
tranTotal atmospheric transmittance1
windirAncillary wind direction relative to North (from NCEP, meteorological convention) that is used in surface roughness correctiondegree
winspdAncillary sea surface wind speed from CCMP NRT that is used in surface roughness correctionm s-1
zangOrbital position angle of S/C. 0 is South. 90 is equator ascending. 180 is North. 270 is equator descending.degree
USER'S GUIDE
ANOMALIES
GENERAL DOCUMENTATION
DATA CITATION POLICY
DATA RECIPE
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 Remote Sensing Systems (RSS). 2024. SMAP Sea Surface Salinity Products. Ver. 6.0. PO.DAAC, CA, USA. Dataset accessed [YYYY-MM-DD] at https://doi.org/10.5067/SMP60-2SNRT

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For more information see Data Citations and Acknowledgments.

Journal Reference Meissner, T. and F. J. Wentz, 2018: Remote Sensing Sytems SMAP Ocean Surface Salinities, Version 4.0 validated release. Remote Sensing Systems, Santa Rosa, CA, USA.

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VersionDatasetVersion DateStatus
6.0RSS SMAP Level 2C Sea Surface Salinity V6.0 Validated Dataset2024-01-08ACTIVE2024-01-08T18:42:00.000Z
6.0RSS SMAP Level 2C Sea Surface Salinity NRT V6.0 Validated Dataset2024-01-08ACTIVE2024-01-08T18:49:00.000Z
5.3RSS SMAP Level 2C Sea Surface Salinity V5.3 Evaluation Dataset2024-04-16COMPLETE2024-04-16T15:59:00.000Z
5.0RSS SMAP Level 2C Sea Surface Salinity V5.0 Validated Dataset2022-07-19ACTIVE2022-07-19T17:30:00.000Z
4.0RSS SMAP Level 2C Sea Surface Salinity V4.0 Validated Dataset2021-09-01ACTIVE2021-09-01T15:58:00.000Z
3.0RSS SMAP Level 2 Sea Surface Salinity V3.0 40km Validated DatasetPresentRETIRED.
2.0RSS SMAP Level 2C Sea Surface Salinity V2.0 Validated Dataset2024-03-20RETIRED.2024-03-20T15:30:00.000Z