N: 66.15 S: -66.15 E: 180 W: -180
Description
The Sensory Geophysical Data Record (SGDR) files contain full accuracy altimeter data, with a high precision orbit (accuracy ~1.5 cm). The instruments on Jason-1 make direct observations of the following quantities: altimeter range, significant wave height, ocean radar backscatter cross-section (a measure of wind speed), ionospheric electron content (derived by a simple formula), tropospheric water content, mean sea surface, and position relative to the GPS satellite constellation. The SGDR contain all relevant corrections needed to calculate the sea surface height. It also contains the 20Hz waveforms that are required for retracking. The SGDR is an expert level product, if you do not require the waveforms then the GDR/GPN or GPR will be more suited for your needs.
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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 |
|---|---|---|---|---|---|---|---|
| rad_land_frac_238 | radiometer 23.8 GHz antenna gain weighted land fraction in main beam | % | short | 32767 | N/A | 0.01 | N/A |
| rad_land_frac_340 | radiometer 34.0 GHz antenna gain weighted land fraction in main beam | % | short | 32767 | N/A | 0.01 | N/A |
| rad_liquid_water | Should not be used over land. | kg/m^2 | short | 32767 | N/A | 0.01 | N/A |
| rad_rain_flag | See Jason-1 User Handbook. The radiometer rain flag indicates where the radiometer wet troposphere path delay (rad_wet_tropo_corr) is invalid due to rain contamination | N/A | byte | 127 | N/A | 1 | N/A |
| rad_sea_ice_flag | See Jason-1 User Handbook. The radiometer sea ice flag indicates where the radiometer wet troposphere path delay (rad_wet_tropo_corr) is invalid due to sea ice contamination | N/A | byte | 127 | N/A | 1 | N/A |
| rad_state_flag_oper | Side A nominal; Side B redundancy | N/A | byte | 127 | N/A | 1 | N/A |
| rad_surf_type | The radiometer surface type flag is applicable to the radiometer wet troposphere path delays provided by rad_wet_tropo_corr. A value of 0 indicates that open ocean processing is used to compute the path delay, 1 indicates coastal processing is used, and 2 indicates the path delay is invalid due to land | N/A | byte | 127 | N/A | 1 | N/A |
| rad_water_vapor | Should not be used over land. | kg/m^2 | short | 32767 | N/A | 0.1 | N/A |
| rad_wet_tropo_corr | A wet tropospheric correction must be added (negative value) to the instrument range to correct this range measurement for wet tropospheric range delays of the radar pulse | m | short | 32767 | N/A | 0.0001 | N/A |
| rain_flag | See Jason-1 User Handbook | N/A | byte | 127 | N/A | 1 | N/A |
| range_20hz_c | All instrumental corrections included, i.e. distance antenna-COG (cog_corr), USO drift correction (uso_corr), internal path correction (internal_path_delay_corr_c), Doppler correction (doppler_corr_c), modeled instrumental errors correction (modeled_instr_corr_range_c) and system bias. range_20hz_c updated to account for reference plane and internal path delay | m | float | 1.0E+30 | N/A | 1 | N/A |
| range_20hz_ku | All instrumental corrections included, i.e. distance antenna-COG (cog_corr), USO drift correction (uso_corr), internal path correction (internal_path_delay_corr_ku), Doppler correction (doppler_corr_ku), modeled instrumental errors correction (modeled_instr_corr_range_ku) and system bias. range_20hz updated to account for reference plane and internal path delay | m | float | 1.0E+30 | N/A | 1 | N/A |
| range_c | All instrumental corrections included, i.e. distance antenna-COG (cog_corr), USO drift correction (uso_corr), internal path correction (internal_path_delay_corr_c), Doppler correction (doppler_corr_c), modeled instrumental errors correction (modeled_instr_corr_range_c) and system bias. range_c updated to account for reference plane and internal path delay | m | float | 1.0E+30 | N/A | 1 | N/A |
| range_ku | All instrumental corrections included, i.e. distance antenna-COG (cog_corr), USO drift correction (uso_corr), internal path correction (internal_path_delay_corr_ku), Doppler correction (doppler_corr_ku), modeled instrumental errors correction (modeled_instr_corr_range_ku) and system bias. range updated to account for reference plane and internal path delay | m | float | 1.0E+30 | N/A | 1 | N/A |
| range_numval_c | number of valid points for C band range | count | byte | 127 | 0 to 20 | 1 | N/A |
| range_numval_ku | number of valid points for Ku band range | count | byte | 127 | 0 to 20 | 1 | N/A |
| range_rms_c | Compression of C-band high rate elements is preceded by a detection of outliers. Only valid high-rate values are used to compute this element | m | short | 32767 | N/A | 0.0001 | N/A |
| range_rms_ku | Compression of Ku-band high rate elements is preceded by a detection of outliers. Only valid high-rate values are used to compute this element | m | short | 32767 | N/A | 0.0001 | N/A |
| range_used_20hz_c | Map of valid points used to compute the 1-Hz C-band altimeter range | N/A | short | 127 | N/A | 1 | N/A |
| range_used_20hz_ku | Map of valid points used to compute the 1-Hz Ku-band altimeter range | N/A | short | 127 | N/A | 1 | N/A |
| scaling_factor_20hz_c | This scaling factor represents the backscatter coefficient for a C-band waveform amplitude equal to 1. It is a raw value accounting for AGC 20Hz correction and internal calibration correction. All other correction are not applied (ie atmospheric attenuation, modeled instrumental errors correction and system bias) | dB | int | 2147483647 | N/A | 0.01 | N/A |
| scaling_factor_20hz_ku | This scaling factor represents the backscatter coefficient for a Ku-band waveform amplitude equal to 1. It is a raw value accounting for AGC 20Hz correction and internal calibration correction. All other correction are not applied (ie atmospheric attenuation, modeled instrumental errors correction and system bias) | dB | int | 2147483647 | N/A | 0.01 | N/A |
| sea_state_bias_c | Computed using wind speed from sigma0 using updated atmospheric attenuation values. A sea state bias correction must be added (negative value) to the instrument range to correct this range measurement for sea state delays of the radar pulse. This element should not be used over land. See Jason-1 User Handbook | m | short | 32767 | N/A | 0.0001 | N/A |
| sea_state_bias_ku | Computed using wind speed from sigma0 using updated atmospheric attenuation values. A sea state bias correction must be added (negative value) to the instrument range to correct this range measurement for sea state delays of the radar pulse. This element should not be used over land. See Jason-1 User Handbook | m | short | 32767 | N/A | 0.0001 | N/A |
| sig0_20hz_c | All instrumental corrections included, excepted the system bias, i.e. AGC instrumental errors correction, internal calibration correction (internal_corr_sig0_c), modeled instrumental errors correction (modeled_instr_corr_sig0_c) and atmospheric attenuation (atmos_corr_sig0_c) | dB | short | 32767 | N/A | 0.01 | N/A |
| sig0_20hz_ku | All instrumental corrections included, excepted the system bias, i.e. AGC instrumental errors correction, internal calibration correction (internal_corr_sig0_ku), modeled instrumental errors correction (modeled_instr_corr_sig0_ku) and atmospheric attenuation (atmos_corr_sig0_ku) | dB | short | 32767 | N/A | 0.01 | N/A |
| sig0_c | All instrumental corrections included, excepted the system bias, i.e. AGC instrumental errors correction, internal calibration correction (internal_corr_sig0_c), modeled instrumental errors correction (modeled_instr_corr_sig0_c) and atmospheric attenuation (atmos_corr_sig0_c) | dB | short | 32767 | N/A | 0.01 | N/A |
| sig0_ku | All instrumental corrections included, excepted the system bias, i.e. AGC instrumental errors correction, internal calibration correction (internal_corr_sig0_ku), modeled instrumental errors correction (modeled_instr_corr_sig0_ku) and atmospheric attenuation (atmos_corr_sig0_ku) | dB | short | 32767 | N/A | 0.01 | N/A |
| sig0_numval_c | number of valid points used to compute C backscatter coefficient | count | byte | 127 | 0 to 20 | 1 | N/A |
| sig0_numval_ku | number of valid points used to compute Ku backscatter coefficient | count | byte | 127 | 0 to 20 | 1 | N/A |
| sig0_rms_c | Compression of C-band high rate elements is preceded by a detection of outliers. Only valid high-rate values are used to compute this element | dB | short | 32767 | N/A | 0.01 | N/A |
| sig0_rms_ku | Compression of Ku-band high rate elements is preceded by a detection of outliers. Only valid high-rate values are used to compute this element | dB | short | 32767 | N/A | 0.01 | N/A |
| sig0_used_20hz_c | Map of valid points used to compute the 1-Hz C-band backscatter coefficient | N/A | byte | 127 | N/A | 1 | N/A |
| sig0_used_20hz_ku | Map of valid points used to compute the 1-Hz Ku-band backscatter coefficient | N/A | byte | 127 | N/A | 1 | N/A |
| solid_earth_tide | Calculated using Cartwright and Tayler tables and consisting of the second and third degree constituents. The permanent tide (zero frequency) is not included. See Jason-1 User Handbook | m | short | 32767 | N/A | 0.0001 | N/A |
| ssha | = altitude of satellite (alt) - Ku band corrected altimeter range (range_ku) - altimeter ionospheric correction on Ku band (iono_corr_alt_ku) - model dry tropospheric correction (model_dry_tropo_corr) - radiometer wet tropospheric correction (rad_wet_tropo_corr) - sea state bias correction in Ku band (sea_state_bias_ku) - solid earth tide height (solid_earth_tide) - geocentric ocean tide height solution 1 (ocean_tide_sol1) - geocentric pole tide height (pole_tide) - inverted barometer height correction (inv_bar_corr) - high frequency fluctuations of the sea surface topography (hf_fluctuations_corr for I/GDR off line products only) - mean sea surface (mean_sea_surface). Set to default if the altimeter surface type (surface_type) is set to 1, 2, or 3 (lake_enclosed_sea, ice, or land) | m | short | 32767 | N/A | 0.001 | N/A |
| surface_type | Computed using a DTM2000 file: 0 = open oceans or semi-enclosed seas; 1 = enclosed seas or lakes; 2 = continental ice; 3 = land. See Jason-1 User Handbook | N/A | byte | 127 | N/A | 1 | N/A |
| surface_type_globcover | Computed from a mask built with MODIS and GlobCover data, 0 = Open ocean; 1 = Land; 2 = Continental waters; 3 = Aquatic vegetation; 4 = Continental ice and snow; 5 = Floating ice; 6 = Salted basin. See Jason-1 User Handbook | N/A | byte | 127 | N/A | 1 | N/A |
| swh_20hz_c | All instrumental corrections included, i.e. modeled instrumental errors correction (modeled_instr_corr_swh_c) and system bias | m | short | 32767 | N/A | 0.001 | N/A |
| swh_20hz_ku | All instrumental corrections included, i.e. modeled instrumental errors correction (modeled_instr_corr_swh_ku) and system bias | m | short | 32767 | N/A | 0.001 | N/A |
| swh_c | All instrumental corrections included, i.e. modeled instrumental errors correction (modeled_instr_corr_swh_c) and system bias | m | short | 32767 | N/A | 0.001 | N/A |
| swh_ku | All instrumental corrections included, i.e. modeled instrumental errors correction (modeled_instr_corr_swh_ku) and system bias | m | short | 32767 | N/A | 0.001 | N/A |
| swh_numval_c | number of valid points used to compute C significant waveheight | count | short | 127 | 0 to 20 | 1 | N/A |
| swh_numval_ku | number of valid points used to compute Ku significant waveheight | count | short | 127 | 0 to 20 | 1 | N/A |
| swh_rms_c | Compression of C-band high rate elements is preceded by a detection of outliers. Only valid high-rate values are used to compute this element | m | short | 32767 | N/A | 0.001 | N/A |
| swh_rms_ku | Compression of Ku-band high rate elements is preceded by a detection of outliers. Only valid high-rate values are used to compute this element | m | short | 32767 | N/A | 0.001 | N/A |
| swh_used_20hz_c | Map of valid points used to compute the 1-Hz C-band significant waveheight | N/A | short | 127 | N/A | 1 | N/A |
| swh_used_20hz_ku | Map of valid points used to compute the 1-Hz Ku-band significant waveheight | N/A | short | 127 | N/A | 1 | N/A |
| ta_187 | 18.7 GHz antenna temperature | K | short | 32767 | N/A | 0.01 | N/A |
| ta_238 | 23.8 GHz antenna temperature | K | short | 32767 | N/A | 0.01 | N/A |