The Siple Station experiment ran from 1973-1988, during which time
a long horizontal ELF transmitter was erected over a thick ice
sheet in Antarctica, described by Raghuram et al [1974]. The
transmitter broadcast tones and frequency ramps to probe the
magnetosphere’s excitation and response to injected ELF/VLF
signals, including amplification and triggered emissions from
wave-particle interactions, along with natural signals like
whistlers and chorus. Receivers were setup at Siple station (75.93
deg. S, 84.25 deg. W geographic, corresponding to an invariant
latitude of 60.4 deg. S, at L = 4.2), and
near the geomagnetic conjugate point (first at Roberval, Quebec,
Canada (48.52 deg. N, 72.23 deg. W) and in 1986
near Lake Mistissini, Canada (50.42 deg. N, 73.87 deg. W)). Complete results of the Siple
station experiment are summarized in Helliwell [1988] but analysis
work on this dataset continued well after the experiment
ended. These data were originally stored on Ampex magnetic tapes,
then converted over to a digitized format with some error
correction applied as described by Li et al [2014].
The sampling rate of these data are 25 kHz.
The filename naming convention is:
XXYYMMDDHHMMSS_ACC.mat
where
XX - Station ID
YY - Year
MM - Month
DD - Day
HH - Hour
MM - Minute
SS - Second
A - Sampling rate. 0 for 100 kHz sampled data (VLF), 1 for 1 MHz
sampled data (LF), 2 for 25 kHz sampled data (Siple station
experiment).
CC - 00 for N/S channel, 01 for E/W channel
Version:2.3.1
The Siple Station experiment ran from 1973-1988, during which time
a long horizontal ELF transmitter was erected over a thick ice
sheet in Antarctica, described by Raghuram et al [1974]. The
transmitter broadcast tones and frequency ramps to probe the
magnetosphere’s excitation and response to injected ELF/VLF
signals, including amplification and triggered emissions from
wave-particle interactions, along with natural signals like
whistlers and chorus. Receivers were setup at Siple station (75.93
deg. S, 84.25 deg. W geographic, corresponding to an invariant
latitude of 60.4 deg. S, at L = 4.2), and
near the geomagnetic conjugate point (first at Roberval, Quebec,
Canada (48.52 deg. N, 72.23 deg. W) and in 1986
near Lake Mistissini, Canada (50.42 deg. N, 73.87 deg. W)). Complete results of the Siple
station experiment are summarized in Helliwell [1988] but analysis
work on this dataset continued well after the experiment
ended. These data were originally stored on Ampex magnetic tapes,
then converted over to a digitized format with some error
correction applied as described by Li et al [2014].
The sampling rate of these data are 25 kHz.
The filename naming convention is:
XXYYMMDDHHMMSS_ACC.mat
where
XX - Station ID
YY - Year
MM - Month
DD - Day
HH - Hour
MM - Minute
SS - Second
A - Sampling rate. 0 for 100 kHz sampled data (VLF), 1 for 1 MHz
sampled data (LF), 2 for 25 kHz sampled data (Siple station
experiment).
CC - 00 for N/S channel, 01 for E/W channel
Role | Person | StartDate | StopDate | Note | |
---|---|---|---|---|---|
1. | ArchiveSpecialist | spase://SMWG/Person/Morris.Cohen |
Sampling rate of the data, 25 kHz.