N: 90 S: -90 E: 180 W: -180
Description
The RSS SMAP level 2C sea surface salinity 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 orbital/swath data on sea surface salinity (SSS) derived from the NASA's Soil Moisture Active Passive (SMAP) mission. The SMAP satellite was launched on 31 January 2015
with a near-polar orbit at an inclination of 98 degrees and an altitude of 685 km. It has an ascending node time of 6 pm and is sun-synchronous. With its 1000km swath, SMAP achieves global coverage in approximately 3 days, but has an exact orbit repeat cycle of 8 days. Malfunction of the SMAP scatterometer on 7 July, 2015, has necessitated the use of collocated wind speed, primarily from WindSat, for the surface roughness correction required for the surface salinity retrieval.
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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.
The SMAP-SSS L2C product includes data for a range of parameters: derived sea surface salinity (SSS) with SSS-uncertainty, brightness temperatures for each radiometer polarization, antenna temperatures, collocated wind speed, data and ancillary reference surface salinity data from HYCOM, rain rate, quality flags, and navigation data.
Each data file covers one 98-minute orbit (15 files per day), is available in netCDF-4 file format with about 4 days l
atency.
Data begins on April 1,2015 and is ongoing. Observations are global in extent with an approximate spatial resolution of 40KM. Note that while a SSS 40KM variable is also included in the product for most open ocean applications, The standard product of the SMAP Version 6.0 release is the smoothed salinity product with a spatial resolution of approximately 70 km.
Product Summary
Citation
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Documents
USER'S GUIDE
ALGORITHM THEORETICAL BASIS DOCUMENT (ATBD)
ANOMALIES
SCIENCE DATA PRODUCT SOFTWARE DOCUMENTATION
DATA CITATION GUIDELINES
Variables
Variables are a set of physical properties whose values determine the characteristics or behavior of something. For example, temperature and pressure are variables of the atmosphere. Parameters and variables can be used interchangeably. Variable level attributes provide individual information for each variable.
The Name in this table is the variable name. Fill value indicates missing or undefined data points in a variable. Valid range is the range of values the variable can store. Scale factor is used to increase or decrease the size of an object and can be used to correct for distortion. For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor |
|---|---|---|---|---|---|---|
| alpha | Scan angle: +90 is left of forward. +270 is right of forward. | degree | float | -9999 | 0 to 360 | 1 |
| anc_sea_ice_flag | ancillary sea-ice detection indicator | 1 | byte | 0 | N/A | 1 |
| cellat | Latitude of OI Earth grid cell | degrees_north | float | -9999 | -90 to 90 | 1 |
| cellon | Longitude of OI Earth grid cell | degrees_east | float | -9999 | 0 to 360 | 1 |
| dtb_land_correction | TA land correction applied at TOA. Pol basis V,H | Kelvin | float | -9999 | N/A | 1 |
| dtb_sea_ice_correction | TB sea-ice correction applied at TB SUR 0. Pol basis V,H | Kelvin | float | -9999 | N/A | 1 |
| dtemp_ant | Empirical correction to physical temperature of reflector. Pol basis V,H | Kelvin | float | -9999 | N/A | 1 |
| eaa | Azimuthal look angle relative to North | degree | float | -9999 | 0 to 360 | 1 |
| eia | Earth incidence angle | degree | float | -9999 | 0 to 90 | 1 |
| fland | land fraction within footprint | 1 | float | -9999 | 0 to 1 | 1 |
| gallat | Latitudinal (polar) angle of specular reflection ray in ECI2000 | degree | float | -9999 | -90 to 90 | 1 |
| gallon | Longitudinal (azimuthal) angle of specular reflection ray in ECI2000 | degree | float | -9999 | 0 to 360 | 1 |
| gice_est | estimated sea ice fraction weighted by antenna gain | 1 | float | -9999 | 0 to 1 | 1 |
| gland | land fraction weighted by antenna gain | 1 | float | -9999 | 0 to 1 | 1 |
| iqc_flag | 32-bit quality control flag | 1 | int | 1 | N/A | 1 |
| monglt | Moon glint angle | degree | float | -9999 | -180 to 180 | 1 |
| pra | Polarization basis rotation angle (geometric part) | degree | float | -9999 | -90 to 90 | 1 |
| pratot_exp | Expected total polarization basis rotation angle: Faraday rotation (from external TEC) + geometric | degree | float | -9999 | -90 to 90 | 1 |
| rain | IMERG rain rate. Resampled to SMAP resolution. | mm h-1 | float | -9999 | 0 to 25 | 1 |
| sea_ice_zones | sea-ice contamination zones | 1 | byte | 7 | 0 to 6 | 1 |
| solar_flux | Ancillary solar flux (from NOAA SWPC) | 1e-22 W m-2 Hz-1 | float | -9999 | N/A | 1 |
| sss_ref | Reference sea surface salinity from HYCOM | 1e-3 | float | -9999 | 0 to 45 | 1 |
| sss_smap | SMAP sea surface salinity smoothed to approx 70km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 |
| sss_smap_40km | SMAP sea surface salinity at original 40km resolution | 1e-3 | float | -9999 | 0 to 45 | 1 |
| 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 |
| 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 |
| 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 |
| 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 |
| sunglt | Sun glint angle. Negative value means that sun ray pierces the Earth. | degree | float | -9999 | -180 to 180 | 1 |
| sun_alpha | Sun azimuth angle in S/C coordinate system | degree | float | -9999 | 0 to 360 | 1 |
| sun_beta | Sun zenith angle in S/C coordinate system | degree | float | -9999 | 0 to 180 | 1 |
| surtep | Ancillary sea surface temperature (from CMC) | Kelvin | float | -9999 | 0 to 313.15 | 1 |
| ta_ant | unfiltered antenna temperature. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 |
| 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 |
| 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 |
| ta_ant_filtered | RFI filtered antenna temperature. Pol basis V,H,S3,S4 | Kelvin | float | -9999 | 0 to 330 | 1 |
| 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 |
| ta_gal_dir | TA of direct galaxy intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 |
| ta_gal_ref | TA of reflected galaxy intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 |
| ta_sun_dir | TA of direct sun intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 |
| ta_sun_ref | TA of reflected sun intrusion. Pol basis I,Q,S3 | Kelvin | float | -9999 | N/A | 1 |
| tbdw | Atmospheric downwelling brightness temperature | Kelvin | float | -9999 | N/A | 1 |
| tbup | Atmospheric upwelling brightness temperature | Kelvin | float | -9999 | N/A | 1 |
| tb_consistency | sqrt(chi2) of MLE in SSS retrieval | Kelvin | float | -9999 | N/A | 1 |
| 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 |
| 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 |
| 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 |
| 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 |
| 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 |
| 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 |