Data Set Information
|
DATA_SET_NAME |
VG2 NEP PWS RAW EXPERIMENT WAVEFORM 60MS V1.0
|
DATA_SET_ID |
VG2-N-PWS-1-EDR-WFRM-60MS-V1.0
|
NSSDC_DATA_SET_ID |
|
DATA_SET_TERSE_DESCRIPTION |
Voyager 2 60 msec electric field waveform sample data from the
Voyager 2 Plasma Wave Receiver (PWS) waveform receiver during
the Neptune encounter from 1990-06-06 to 1990-09-27.
|
DATA_SET_DESCRIPTION |
Data Set Overview
=================
This data set consists of electric field waveform samples from the
Voyager 2 Plasma Wave Receiver waveform receiver obtained during
the Neptune encounter. The waveforms are collections of 4-bit
samples of the electric field measured by the dipole electric antenna
at a rate of 28,800 samples per second. 1600 samples are collected
in 55.56 msec followed by a 4.44-msec gap. Each 60-msec interval
constitutes a line of waveform samples. The data set includes about 271
frames of waveform samples consisting of up to 800 lines, each. The
telemetry format for the waveform data is identical to that for
images, hence the use of line and frame as constructs in describing
the form of the data. The waveform is sampled through a bandpass
filter with a passband of 40 Hz to 12 kHz. The 4-bit samples
provide sixteen digital values of the electric field with a
linear amplitude scale, but the amplitude scale is arbitrary
because of the automatic gain control used in the waveform
receiver. The instantaneous dynamic range afforded by the 4
bit samples is about 23 db, but the automatic gain control allows
the dominant signal in the passband to be set at the optimum
level to fit within the instantaneous dynamic range. With the gain
control, the overall dynamic range of the waveform receiver
is about 100 db. The automatic gain control gain setting is not
returned to the ground, hence, there is no absolute calibration
for the data. However, by comparing the waveform spectrum derived
by Fourier transforming the waveform to the spectrum provided by
the spectrum analyzer data, an absolute calibration may be
obtained in most cases. The data may be plotted in raw form to
show the actual waveform; this is useful for studying events such
as dust impacts on the spacecraft. But the normal method of
analyzing the waveform data is by Fourier transforming the samples
from each line to arrive at an amplitude versus frequency spectrum.
By stacking the spectra side-by-side in time order, a frequency-
time spectrogram can be produced.
Additional information about this dataset and the instrument which
produced it can be found elsewhere in this catalog. An overview of
the data in this data set can be found in Gurnett et al. [1989] and
a complete instrument description can be found in Scarf and Gurnett
[1977].
Parameters
==========
Derived Parameters
------------------
Sampling Parameter Name : time
Sampling Parameter Resolution : 0.000034722 seconds
Minimum Sampling Parameter : n/a
Maximum Sampling Parameter : n/a
Sampling Parameter Interval : 0.000034722 seconds
Minimum Available Sampling Interval : 0.000034722 seconds
Data Set Parameter Name : plasma wave waveform
Noise Level : 0.000005
Data Set Parameter Unit : volt/meter (Data not
absolutely
calibrated)
Plasma wave waveform: A plasma wave waveform is a time series of
measurements of the electric or magnetic field component of the
wave spectrum taken through a broadband filter. The temporal
sample rate is normally such that samples are made at more than
twice the analysis filter bandwidth. A typical waveform will
consist of the order of 1000 contiguous samples of between 4 and
12 bits each. For a 10-kHz analysis bandwidth, the sample rate
would normally be approximately 25 kHz or 25,000 samples/second.
Once received, the waveforms are typically Fourier transformed in
order to provide an amplitude versus frequency spectrum across
the analysis bandwidth. The sample rate, then, is required to be
at least a factor of two greater than the filter bandwidth in
order to avoid aliasing in the transformed spectrum. The spectra
can be stacked side-by-side in time to build a frequency-time
spectrogram (that is, amplitude as a function of time and
frequency) in order to identify the temporal and spectral
variations in the wave spectrum. Alternately, the untransformed
time series can be used to study the details of the waveform.
This has been useful for measuring small-scale structures in the
plasma and for identifying the signature of micron-sized dust
impact on the spacecraft.
Measured Parameters
-------------------
Electric field component: A measured parameter equaling the electric
field strength (e.g. in milli-volts per meter) along a particular
axis direction.
Wave magnetic field intensity: A measured parameter equaling the
magnetic field strength in a specific frequency passband (in MKS
unit: volts/meter) measured in a single sensor or antenna.
Wave electric field intensity: A measured parameter equaling the
electric field strength in a specific frequency passband (in MKS
unit: volts/meter) measured in a single sensor or antenna.
Processing
==========
The data files in this data set were created using the 'CDREF'
software.
CDREF
-----
Node ID : IMAGING
Software Release Date : 1990-04-07
Cognizant Full Name : MR. JASON J. HYON
CDREF is primarily a data format translation routine which is used
to convert Voyager PWS EDR tape files to CD-ROM files. CDREF is
written in FORTRAN and is not available for public use. The EDR,
or Engineering Data Records, are produced at Multi-mission Image
Processing Laboratory at JPL as the uncalibrated, full-resolution
PWS spectrum analyzer data set.
The CD files contain uncalibrated, full-resolution PWS data with
minimal ancillary data in a simplified format which may be used in
CDROM production.
|
DATA_SET_RELEASE_DATE |
1990-09-01T00:00:00.000Z
|
START_TIME |
1989-06-06T02:16:56.000Z
|
STOP_TIME |
1989-09-27T05:52:43.000Z
|
MISSION_NAME |
VOYAGER
|
MISSION_START_DATE |
1972-07-01T12:00:00.000Z
|
MISSION_STOP_DATE |
N/A (ongoing)
|
TARGET_NAME |
NEPTUNE
|
TARGET_TYPE |
PLANET
|
INSTRUMENT_HOST_ID |
VG2
|
INSTRUMENT_NAME |
PLASMA WAVE RECEIVER
|
INSTRUMENT_ID |
PWS
|
INSTRUMENT_TYPE |
PLASMA WAVE SPECTROMETER
|
NODE_NAME |
Planetary Plasma Interactions
|
ARCHIVE_STATUS |
ARCHIVED
|
CONFIDENCE_LEVEL_NOTE |
Confidence Level Overview
=========================
This data set includes all available waveform receiver data obtained
during the Neptune encounter. There has been no attempt
to clean various interference signals from the data. Most of these
can normally be easily seen in frequency-time spectrograms as
narrowband, fixed-frequency tones. The most common include narrow-
band tones at 2.4 and 4.8 kHz which are power supply harmonics.
There is sometimes a tone near 1.7 kHz which is associated with
the operation of the spacecraft gyros. The spacecraft tape
recorder results in a rather intense band in the frequency range
of a few hundred Hz. There are few times when the data in this
frequency range can be used. However, there are times when the
real signals in this frequency range can exceed the intensity of
the interference sufficiently so that the frequency range near
a few hundred Hz can be used. Use of the spectrum analyzer data
can be of use to determine when these time periods occur. The
stepper motor of the LECP instrument also interferes in the
frequency range of a few hundred Hz, but for periods of a few
seconds.
The LECP interference is very intense and captures the automatic
gain control so that real signals, even where there is no
interference, will appear to decrease in amplitude until the LECP
interference fades in amplitude. The PLS instrument periodically
interferes at 400 Hz and odd harmonics because of a 400-Hz square
wave used to modulate a grid in the detector. The PLS interference
lasts for several seconds and ends abruptly. Telemetry errors
result in a fairly graceful degradation of the waveform data.
Assuming the telemetry errors are randomly occurring bursts, they
typically appear as an enhanced background level in the spectrum.
Since the bursts are short, their Fourier transform is a broadband
spectrum. When looking for relatively narrowband features or
features with distinct frequency-time characteristics, the result
of the bursts simply reduce the signal-to-noise in the spectrum.
One way of reducing the effect of burst telemetry errors is to pass
the waveform data through a low-pass filter to despike it, prior to
running the Fourier transform. The waveform data is not subject
to the negative effects of the failure in the Voyager 2 Flight
Data System which reduces the sensitivity of the spectrum analyzer
and affects the calibration above 1 kHz. In fact, use of the 1 -
12 kHz waveform data is an effective way of avoiding the problems
with the spectrum analyzer data in this frequency range.
Data Quality and Coverage
=========================
--------------------------------------------------------------------
Table 1. Data Quality ID Descriptions
--------------------------------------------------------------------
ID Description
--------------------------------------------------------------------
-1 no attempt has been made to specify a data quality for this
time range
1 Contamination removed by deleting measurements which are
affected. Some contamination may still be present to avoid
deleting too many data points. Remaining LECP contamination
will appear as periodic bursts of noise in one or more
channels in the range 100 Hertz to about 1 kiloHertz.
--------------------------------------------------------------------
Table 2. Data Contamination ID Descriptions
--------------------------------------------------------------------
ID Description
--------------------------------------------------------------------
-1 no evaluation of possible contamination has been made
1 Contamination code 01 refers to contamination by the LECP
stepper motor and PLS grid modulation which causes periodic
spikes in the spectrum analyzer data particularly in the
frequency range 100 Hertz to about 1 kiloHertz.
|
CITATION_DESCRIPTION |
Kurth, W.S., VG2-N-PWS-1-EDR-WFRM-60MS-V1.0,
VG2 NEP PWS RAW EXPERIMENT WAVEFORM 60MS V1.0,
NASA Planetary Data System, 1990.
|
ABSTRACT_TEXT |
This data set consists of electric field waveform samples from the
Voyager 2 Plasma Wave Receiver waveform receiver obtained during
the Neptune encounter. The waveforms are collections of 4-bit
samples of the electric field measured by the dipole electric antenna
at a rate of 28,800 samples per second. 1600 samples are collected
in 55.56 msec followed by a 4.44-msec gap. Each 60-msec interval
constitutes a line of waveform samples. The data set includes about 271
frames of waveform samples consisting of up to 800 lines, each.
|
PRODUCER_FULL_NAME |
DR. WILLIAM S. KURTH
|
SEARCH/ACCESS DATA |
Planetary Plasma Interactions Website
|
|