Data Access
Amplitude and phase time series of low frequency standard radio transmitter signals at 19.80(NWC), 21.40(NPM), 24.80(NLK), 25.20(NDK), 37.50(NRK), 40.75(NAU), and 60.00kHz(WWVB) received at the Athabasca station, Canada. Variations in the phase and amplitude reflect changes of the ionization state in the lower ionosphere which is caused by energetic electron precipitation from inner magnetosphere (radiation belt), solar x-rays, lightning dischanges, and so on.
Version:2.5.0
Amplitude and phase time series of low frequency standard radio transmitter signals at 19.80(NWC), 21.40(NPM), 24.80(NLK), 25.20(NDK), 37.50(NRK), 40.75(NAU), and 60.00kHz(WWVB) received at the Athabasca station, Canada. Variations in the phase and amplitude reflect changes of the ionization state in the lower ionosphere which is caused by energetic electron precipitation from inner magnetosphere (radiation belt), solar x-rays, lightning dischanges, and so on.
Role | Person | StartDate | StopDate | Note | |
---|---|---|---|---|---|
1. | PrincipalInvestigator | spase://IUGONET/Person/Fuminori.Tsuchiya | |||
2. | MetadataContact | spase://IUGONET/Person/Manabu.Yagi |
time label in CDF_EPOCH (the number of milliseconds since 01-Jan-0000) for the 30 sec data
Year, month, day, hour, minute, and second of each time frame for the 30 sec data
Amplitude time series of standard radio signals at 19.80, 21.40, 24.80, 25.20, 37.50, 40.75, and 60.00kHz
Phase time series of standard radio signals at 19.80, 21.40, 24.80, 25.20, 37.50, 40.75, and 60.00kHz