N: 90 S: -90 E: 180 W: -180
Description
The SMAP-SSS level 2C near real-time (NRT) V5.0 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. Data from July 28, 2022 to present, is available with a latency of about 6 hours. The observations are global, provided on a 0.25° fixed Earth grid with an approximate spatial resolution of 70 km. The major differences to the standard version 5.0 data products are: (1) the NRT version of the L1B SMAP antenna temperatures is used, (2) the latest 6-hourly 0.25° wind speed and direction are used for the ancillary wind speed and direction input, (3) the CMC SST from 2 days earlier is used for the ancillary SST input, (4) the sea-ice mask of the 3-day aggregate RSS AMSR-2 Air-Sea Essential Climate Variables (AS-ECV) data set from 2-days earlier is used for the sea-ice flag, (5) no correction for sea-ice contamination is performed, it is recommended to use only SMAP data that are classified to be within sea-ice zone 0 for open ocean scene and no sea-ice contamination.
This RSS SMAP-SSS V5.0 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.
This activity was informed by the Satellite Needs Working Group (SNWG), an interagency effort of the U.S. Government dedicated to identifying and addressing Earth observation needs across U.S. civilian federal agencies.
Product Summary
Citation
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Variables
The table below lists the variables contained within a single granule for this dataset. Variables often contain observed or derived geophysical measurements collected from a variety of sources, including remote sensing instruments on satellite and airborne platforms, field campaigns, in situ measurements, and model outputs. The terms variable, parameter, scientific data set, layer, and band have been used across NASA’s Earth science disciplines; however, variable is the designated nomenclature in NASA’s Common Metadata Repository (CMR). Variable metadata attributes such as Name, Description, Units, Data Type, Fill Value, Valid Range, and Scale Factor allow users to efficiently process and analyze the data. The full range of attributes may not be applicable to all variables. Additional information on variable attributes is typically available in the data, user guide, and/or other product documentation.
For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor | Offset |
|---|---|---|---|---|---|---|---|
| alpha | Scan angle: +90 is left of forward. +270 is right of forward. | degree | float | -9999 | 0 to 360 | 1 | N/A |
| anc_sea_ice_flag | ancillary sea-ice detection indicator | 1 | byte | 0 | N/A | 1 | N/A |
| cellat | Latitude of OI Earth grid cell | degrees_north | float | -9999 | -90 to 90 | 1 | N/A |
| cellon | Longitude of OI Earth grid cell | degrees_east | float | -9999 | 0 to 360 | 1 | N/A |
| dtb_land_correction | TA land correction applied at TOA. Pol basis V,H | Kelvin | float | -9999 | N/A | 1 | N/A |
| dtemp_ant | Empirical correction to physical temperature of reflector. Pol basis V,H | Kelvin | float | -9999 | N/A | 1 | N/A |
| eaa | Azimuthal look angle relative to North | degree | float | -9999 | 0 to 360 | 1 | N/A |
| eia | Earth incidence angle | degree | float | -9999 | 0 to 90 | 1 | N/A |
| fland | land fraction within footprint | 1 | float | -9999 | 0 to 1 | 1 | N/A |
| gallat | Latitudinal (polar) angle of specular reflection ray in ECI2000 | degree | float | -9999 | -90 to 90 | 1 | N/A |
| gallon | Longitudinal (azimuthal) angle of specular reflection ray in ECI2000 | degree | float | -9999 | 0 to 360 | 1 | N/A |
| gland | land fraction weighted by antenna gain | 1 | float | -9999 | 0 to 1 | 1 | N/A |
| iqc_flag | 32-bit quality control flag | 1 | int | 1 | N/A | 1 | N/A |
| monglt | Moon glint angle | degree | float | -9999 | -180 to 180 | 1 | N/A |
| pra | Polarization basis rotation angle (geometric part) | degree | float | -9999 | -90 to 90 | 1 | N/A |
| pratot_exp | Expected total polarization basis rotation angle: Faraday rotation (from external TEC) + geometric | degree | float | -9999 | -90 to 90 | 1 | N/A |
| rain | rain rate. estimated from NCEP could water profiles | mm h-1 | float | -9999 | 0 to 25 | 1 | N/A |
| sea_ice_zones | sea-ice contamination zones | 1 | byte | 7 | 0 to 6 | 1 | N/A |
| solar_flux | Ancillary solar flux (from NOAA SWPC) | 1e-22 W m-2 Hz-1 | float | -9999 | N/A | 1 | N/A |
| sss_ref | Reference sea surface salinity from HYCOM | 1e-3 | float | -9999 | 0 to 45 | 1 | N/A |
| sss_smap | SMAP sea surface salinity smoothed to approx 70km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 | N/A |
| sss_smap_40km | SMAP sea surface salinity at original 40km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 | N/A |
| sss_smap_40km_unc | total formal uncertainty estimate of SMAP sea surface salinity at original 40km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 | N/A |
| sss_smap_40km_unc_comp | formal uncertainty components of SMAP sea surface salinity at original 40km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 | N/A |
| sss_smap_unc | total formal uncertainty estimate of SMAP sea surface salinity smoothed to approx 70km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 | N/A |
| sss_smap_unc_comp | formal uncertainty components of SMAP sea surface salinity smoothed to approx 70km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 | N/A |
| sunglt | Sun glint angle. Negative value means that sun ray pierces the Earth. | degree | float | -9999 | -180 to 180 | 1 | N/A |
| sun_alpha | Sun azimuth angle in S/C coordinate system | degree | float | -9999 | 0 to 360 | 1 | N/A |
| sun_beta | Sun zenith angle in S/C coordinate system | degree | float | -9999 | 0 to 180 | 1 | N/A |
| surtep | Ancillary sea surface temperature (from CMC) | Kelvin | float | -9999 | 0 to 313.15 | 1 | N/A |
| ta_ant | unfiltered antenna temperature. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| ta_ant_calibrated | Antenna temperature after correcting for emissive reflector and TND adjustment. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| ta_ant_exp | Expected (RTM) antenna temperature before any losses. This is to be compared with ta_ant_calibrated. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| ta_ant_filtered | RFI filtered antenna temperature. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| ta_earth | Antenna temperature after correcting for cold space, galaxy, sun, moon. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| ta_gal_dir | TA of direct galaxy intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 | N/A |
| ta_gal_ref | TA of reflected galaxy intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 | N/A |
| ta_sun_dir | TA of direct sun intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 | N/A |
| ta_sun_ref | TA of reflected sun intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 | N/A |
| tbdw | Atmospheric downwelling brightness temperature | Kelvin | float | -9999 | N/A | 1 | N/A |
| tbup | Atmospheric upwelling brightness temperature | Kelvin | float | -9999 | N/A | 1 | N/A |
| tb_consistency | sqrt(chi2) of MLE in SSS retrieval | Kelvin | float | -9999 | N/A | 1 | N/A |
| tb_sur | Brightness temperature at rough ocean surface BEFORE applying roughness correction. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| tb_sur0 | Brightness temperature at flat ocean surface AFTER applying roughness correction. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| tb_sur0_exp | Expected (RTM) at flat ocean surface. SIC added. This is to be compared with tb_sur0, before SIC. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| tb_sur0_sic | Brightness temperature at flat ocean surface after applying roughness correction and sea-ice correction. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| tb_toa | Brightness temperature at top of atmosphere BEFORE applying land correction. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| tb_toa_lc | Brightness temperature at top of atmosphere AFTER applying land correction. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| tb_toi | Brightness temperature at top of ionosphere. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 | N/A |
| TEC | Vertically integrated electron content between surface and S/C | 1e16 m-2 | float | -9999 | N/A | 1 | N/A |