RO Data Description


Data type:

- ionPrf

- igaPrf


ionPrf is one of the data products from FORMOSAT-7/COSMIC-2 occultation observation, which includes the ionospheric electron density profiles, the calibrated TEC, geographic longitude / latitude / altitude at perigees, etc.


igaPrf is another data products derived from ionPrf, which includes corrected electron density profiles and some related observables.


The major difference between ionPrf and igaPrf is: the former is derived from the standard Abel inversion; the latter is derived from the aided-Abel inversion.



ionPrf Profile Data


MSL_alt: Mean sea level altitude of perigee point in km


GEO_lon:Geographic longitude of perigee point in °E


GEO_lat:Geographical latitude of perigee point in °N


TEC_cal:Calibrated occultation TEC below LEO orbit in TECU


ELEC_dens:Electron density in el/cm3



igaPrf Profile Data


MSL_alt:Mean sea level altitude of perigee point in km


GEO_lon:Geographic longitude of perigee point in °E


GEO_lat:Geographical latitude of perigee point in °N


TEC_cal:Calibrated occultation TEC below LEO orbit in TECU


ELEC_dens:Aided electron density in el/cm3


ELEC_dens_orig:Original electron density in el/cm3 (same as ELEC_dens in ionPrf)


ELEC_dens_bg:Background electron density in el/cm3



ionPrf Data Processing


Since FORMOSAT-7/COSMIC-2 provides dual-frequency GNSS occultation and non-occultation observables, the ionospheric electron density profile can be retrieved from two data processings: the excess phase data processing and ionosphere inversion processing.


The former data processing estimates the ionospheric excess phase by the following procedures:

- Read in 1-second sampled dual-frequency GNSS phase observables

- Derive the linear combinataion of the excess phase by linear differencing

- Identify occultation flag (rising/setting) or indicate it if it is an non-occultation event based on the orbital information of GNSS and LEO satellites


The latter processing retrieves the ionospheric electron density profile by the following procedures:

- Read in electron density profiles in ionPrf

- Reconstruct 3-dimensional global electron density field as the background field based on 45-day worth of the profiles

- Convert the calibrated TEC into the corrected (aided) electron density profiles based on the aided-Abel inversion (cf. Chou et al., 2019)



Reference:


Chou, M. Y., C. C. H. Lin, H.-F. Tsai, and C.-Y. Lin (2017), Ionospheric electron density inversion for Global Navigation Satellite Systems radio occultation using aided Abel inversions, J. Geophys. Res. Space Physics, 122, doi:10.1002/2016JA023027.