N: 52 S: 24 E: -82 W: -113
Description
This dataset contains a simulated rasterized water surface elevation and inundation-extent product to be provided by the Surface Water and Ocean Topography (SWOT) mission. SWOT will provide a global coverage but this simulated subset focuses on the North America continent. This is a derived product through resampling the upstream dataset L2_HR_PIXC_V1 and L2_HR_PIXCVEC_V1 onto a uniform grid over the North America continent. A uniform grid is superimposed onto the pixel cloud from the source products, and all pixel-cloud samples within each grid cell are aggregated to produce a single value per raster cell. The raster data are produced geographically fixed tiles at resolutions of 100 m and 250 m in a Universal Transverse Mercator projection grid. Note that this is a simulated SWOT product and not suited for any scientific exploration.
Product Summary
Citation
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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 |
|---|---|---|---|---|---|---|
| cross_track | Approximate cross-track location of the pixel. | m | float | 9.96921E+36 | -75000 to 75000 | 1 |
| crs | UTM zone coordinate reference system. | N/A | string | N/A | N/A | 1 |
| dark_frac | Fraction of pixel water area covered by dark water. | l | float | 9.96921E+36 | -1000 to 10000 | 1 |
| geoid | Geoid height above the reference ellipsoid with a correction to refer the value to the mean tide system, i.e. includes the permanent tide (zero frequency). | m | float | 9.96921E+36 | -150 to 150 | 1 |
| ice_clim_flag | Climatological ice cover flag indicating whether the pixel is ice-covered on the day of the observation based on external climatological information (not the SWOT measurement). Values of 0, 1, and 2 indicate that the pixel is likely not ice covered, may or may not be partially or fully ice covered, and likely fully ice covered, respectively. | N/A | ubyte | 255 | 0 to 2 | 1 |
| ice_dyn_flag | Dynamic ice cover flag indicating whether the surface is ice-covered on the day of the observation based on analysis of external satellite optical data. Values of 0, 1, and 2 indicate that the pixel is not ice covered, partially ice covered, and fully ice covered, respectively. | N/A | ubyte | 255 | 0 to 2 | 1 |
| illumination_time | Time of measurement in seconds in the UTC time scale since 1 Jan 2000 00:00:00 UTC. [tai_utc_difference] is the difference between TAI and UTC reference time (seconds) for the first measurement of the data set. If a leap second occurs within the data set, the attribute leap_second is set to the UTC time at which the leap second occurs. | seconds since 2000-01-01 00:00:00.000 | double | 9.9692099683869E+36 | N/A | 1 |
| illumination_time_tai | Time of measurement in seconds in the TAI time scale since 1 Jan 2000 00:00:00 TAI. This time scale contains no leap seconds. The difference (in seconds) with time in UTC is given by the attribute [illumination_time:tai_utc_difference]. | seconds since 2000-01-01 00:00:00.000 | double | 9.9692099683869E+36 | N/A | 1 |
| inc | Incidence angle. | degrees | float | 9.96921E+36 | 0 to 90 | 1 |
| iono_cor_gim_ka | Equivalent vertical correction due to ionosphere delay. The reported water surface elevation, latitude and longitude are computed after adding negative media corrections to uncorrected range along slant-range paths, accounting for the differential delay between the two KaRIn antennas. The equivalent vertical correction is computed by applying obliquity factors to the slant-path correction. Adding the reported correction to the reported water surface elevation results in the uncorrected pixel height. | m | float | 9.96921E+36 | -0.5 0 | 1 |
| latitude | Latitude [-80,80] (degrees north of equator) of the pixel. | degrees_north | double | 9.9692099683869E+36 | -80 to 80 | 1 |
| layover_impact | Estimate of the water surface elevation error caused by layover. | m | float | 9.96921E+36 | -999999 to 999999 | 1 |
| load_tide_fes | Geocentric load tide height. The effect of the ocean tide loading of the Earth’s crust. | m | float | 9.96921E+36 | -0.2 to 0.2 | 1 |
| load_tide_got | Geocentric load tide height. The effect of the ocean tide loading of the Earth’s crust. This value is reported for reference but is not applied to the reported height. | m | float | 9.96921E+36 | -0.2 to 0.2 | 1 |
| longitude | Longitude [-180,180) (east of the Greenwich meridian) of the pixel. | degrees_east | double | 9.9692099683869E+36 | -180 to 180 | 1 |
| model_dry_tropo_cor | Equivalent vertical correction due to dry troposphere delay. The reported water surface elevation, latitude and longitude are computed after adding negative media corrections to uncorrected range along slant-range paths, accounting for the differential delay between the two KaRIn antennas. The equivalent vertical correction is computed by applying obliquity factors to the slant-path correction. Adding the reported correction to the reported water surface elevation results in the uncorrected pixel height. | m | float | 9.96921E+36 | -3 to -1.5 | 1 |
| model_wet_tropo_cor | Equivalent vertical correction due to wet troposphere delay. The reported water surface elevation, latitude and longitude are computed after adding negative media corrections to uncorrected range along slant-range paths, accounting for the differential delay between the two KaRIn antennas. The equivalent vertical correction is computed by applying obliquity factors to the slant-path correction. Adding the reported correction to the reported water surface elevation results in the uncorrected pixel height. | m | float | 9.96921E+36 | -1 0 | 1 |
| n_area_pix | Number of pixel cloud samples used in water area and water fraction aggregation. | l | uint | 4294967295 | 0 to 999999 | 1 |
| n_wse_pix | Number of pixel cloud samples used in water surface elevation aggregation. | l | uint | 4294967295 | 0 to 999999 | 1 |
| pole_tide | Geocentric pole tide height. The total of the contribution from the solid-Earth (body) pole tide height and the load pole tide height (i.e., the effect of the ocean pole tide loading of the Earth’s crust). | m | float | 9.96921E+36 | -0.2 to 0.2 | 1 |
| raster_qual | Quality flag for raster data. | N/A | ubyte | 255 | 0 to 1 | 1 |
| sig0 | Normalized radar cross section (sigma0) in real, linear units (not decibels). The value may be negative due to noise subtraction. | 1 | float | 9.96921E+36 | -1000 to 10000000 | 1 |
| sig0_uncert | 1-sigma uncertainty in sigma0. The value is provided in linear units. This value is a one-sigma additive (not multiplicative) uncertainty term, which can be added to or subtracted from sigma0. | 1 | float | 9.96921E+36 | 0 to 1000 | 1 |
| solid_earth_tide | Solid-Earth (body) tide height. The zero-frequency permanent tide component is not included. | m | float | 9.96921E+36 | -1 to 1 | 1 |
| water_area | Surface area of the water pixels. | m^2 | float | 9.96921E+36 | -2000000 to 2000000000 | 1 |
| water_area_uncert | 1-sigma uncertainty in the water surface area | m^2 | float | 9.96921E+36 | 0 to 2000000000 | 1 |
| water_frac | Fraction of the pixel that is water. | 1 | float | 9.96921E+36 | -1000 to 10000 | 1 |
| water_frac_uncert | 1-sigma uncertainty in the water fraction. | 1 | float | 9.96921E+36 | 0 to 999999 | 1 |
| wse | Water surface elevation of the pixel above the geoid and after using models to subtract the effects of tides (solid_earth_tide, load_tide_fes, pole_tide). | m | float | 9.96921E+36 | -1500 to 15000 | 1 |
| wse_uncert | 1-sigma uncertainty in the water surface elevation. | m | float | 9.96921E+36 | 0 to 999999 | 1 |
| x | UTM easting coordinate of the pixel. | m | double | 9.9692099683869E+36 | -10000000 to 10000000 | 1 |
| y | UTM northing coordinate of the pixel. | m | double | 9.9692099683869E+36 | -20000000 to 20000000 | 1 |