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2.5-minute averaged magnetic field measurements from Vega 2.
During the cruise phase from Earth to Venus (12/84-06/85) both Vega-1 and Vega-2 spacecraft had one-axis orientation, i.e. the spacecraft X axis was maintained sunward-pointing, while the spacecraft Y and Z axes rotated about the X axis. The spin phase of this rotation was not known, therefore the directions of By and Bz components are unknown. Magnetometer data for this period are presented in spacecraft coordinates as Br (directed radially from spacecraft to the Sun), Bysc, Bzsc. From the providers: "It is proposed to use for analysis of the interplanetary magnetic field during this period the Br component and the total B=sqrt(Bxsc^2+Bysc^2+Bzsc^2). Bysc and Bzsc components are included in the data, but keep in mind that the orientation of these axes is unknown. It can be considered as fixed during periods up to a few hours, so the data can be used to look for IMF discontinues and IMF orientation variations."
After Venus flybys (June, 11-15, 1985) up to Comet Halley (March, 6 and 9, 1986) and sometimes later Vega-1 and Vega-2 had three-axis stabilized orientations. After-Venus magnetic field data are presented in spacecraft-centered solar ecliptic (SE) coordinate system as Br, Bzse, Byse, B, where Br is directed from the spacecraft to the Sun, Bzse is directed along Bz axes of the Solar Ecliptic system (to ecliptic pole), Byse completes the right handed set and B=sqrt(Br^2+By^2+Bz^2).
Use of these data in publications should be accompanied by acknowledgements of the National Space Science Data Center(NSSDC), Space Physics Data Facility(SPDF) and IZMIRAN at Moscow.
| Role | Person | |
|---|---|---|
| 1. | General contact | Valery G. Petrov |
| 2. | Data producer | Dr. Valery A. Styazhkin |
| 3. | Technical contact | Dr. Natalia E. Papitashvili |
| 4. | Metadata contact | Jan Merka |
FTP access to Vega mission data at NSSDC.
Time of observation (year)
Time of observation (month of year)
Time of observation (day of month)
Time of observation (hour of day)
Time of observation (minute)
Time of observation (second)
Magnetic field radial (+ to Sun) component
Magnetic field data are presented in spacecraft coordinates (SC) (before the Venus flyby) or in spacecraft-centered solar ecliptic (SE) coordinate system (after the Venus flyby). In both cases the Br(=Bx) component points towards Sun.
See also the CSflag parameter.
Magnetic field By component
During the cruise phase from Earth to Venus (12/84-06/85) both Vega-1 and Vega-2 spacecraft had one-axis orientation, i.e. the spacecraft X axis was maintained sunward-pointing, while the spacecraft Y and Z axes rotated about the X axis. The spin phase of this rotation was not known, therefore the directions of By and Bz components are unknown.
After-Venus magnetic field data are presented in spacecraft-centered solar ecliptic (SE) coordinate system as Br, Bzse, Byse, B, where Br is directed from the spacecraft to the Sun, Bzse is directed along Bz axes of the Solar Ecliptic system (to ecliptic pole), Byse completes the right handed set and B=sqrt(Br^2+By^2+Bz^2).
See also the CSflag parameter.
Magnetic field Bz component
During the cruise phase from Earth to Venus (12/84-06/85) both Vega-1 and Vega-2 spacecraft had one-axis orientation, i.e. the spacecraft X axis was maintained sunward-pointing, while the spacecraft Y and Z axes rotated about the X axis. The spin phase of this rotation was not known, therefore the directions of By and Bz components are unknown.
After-Venus magnetic field data are presented in spacecraft-centered solar ecliptic (SE) coordinate system as Br, Bzse, Byse, B, where Br is directed from the spacecraft to the Sun, Bzse is directed along Bz axes of the Solar Ecliptic system (to ecliptic pole), Byse completes the right handed set and B=sqrt(Br^2+By^2+Bz^2).
See also the CSflag parameter.
Magnetic field magnitude in nT
Spacecraft radial distance from Sun in AU.
HGI spacecraft position azimuth, degrees.
HGI Spacecraft position elevation, degrees.
Coordinate system flag for magnetic field data.
| Flag | Coordinate system |
|---|---|
| 0 | Spacecraft coordinates |
| 1 | Solar Ecliptic coordinates |
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The magnetometers on Vega 1 and Vega 2 were designed to measure the magnetic field and its low-frequency fluctuations in the cometary and solar wind interaction zone and in interplanetary space. The instrument on each spacecraft consisted of two fluxgate sensor units (one axial and triaxial) mounted 1 m apart on a 2-m boom. The advantage of this dual-sensor fluxgate system is the possibility to determine the spacecraft's stray magnetic field.
The axial unit was oriented along the spacecraft symmetry (X) axis, which was perpendicular to the solar panels and pointed toward the Sun. Each sensor had a dynamic range of ± 100 nT, sensitivity of 0.05 nT (12 bit) and a noise level of 0.01 nT/Hz^(1/2). Magnetic field vectors were measured with a sampling frequency of 10 vectors per second.
The magnetometers operated in three data rate modes:
Cruise phase data were mostly taken in the 2.5-min averaging mode.
Information about the Magnetometer experiment on the Vega 2 mission.
Prof. Willi W. Riedler, Austrian Academy of Sciences, and IZMIRAN.
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Prof. Willi W. Riedler |
| 2. | CoInvestigator | Dr. N. A. Stjazhkin |
| 3. | CoInvestigator | Dr. Ye. G. Yeroshenko |
| 4. | CoInvestigator | Dr. Konrad Schwingenschuh |
| 5. | CoInvestigator | Dr. R. Schmidt |
| 6. | Metadata contact | Jan Merka |
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This spacecraft mission combined a Venus swingby and a Comet Halley flyby. Two identical spacecraft, Vega 1 and Vega 2, were launched December 15 and 21, 1984, respectively. After carrying Venus entry probes to the vicinity of Venus (arrival and deployment of probes were scheduled for June 11-15, 1985), the two spacecraft were retargetted using Venus gravity field assistance to intercept Comet Halley in March 1986. The first spacecraft encountered Comet Halley on March 6, 1986, and the second three days later. The flyby velocity was 77.7 km/s. Although the spacecraft could be targetted with a precision of 100 km, the position of the spacecraft relative to the comet nucleus was estimated to be known only to within a few thousand kilometers. This, together with the problem of dust protection, led to estimated flyby distances of 10,000 km for the first spacecraft and 3000 km for the second.
The spacecraft was three-axis stabilized. Its main features were large solar panels, a high-gain antenna dish, and an automatic pointing platform carrying those experiments that required pointing at the comet nucleus. The automatic platform could rotate through + or -110 deg and + or -40 deg in two perpendicular directions with a pointing accuracy of 5 arc-min and a stability of 1 arc-min/s. It carried the narrow- and the wide-angle camera, the three-channel spectrometer, and the infrared sounder. All other experiments were body-mounted, with the exception of two magnetometer sensors mounted on a 2-m boom and various plasma probes and plasma wavw analyzers mounted on a 5-m boom. The total scientificpayload weighed 125 kg and had a data rate of 65 kbs in fast telemetry mode for encounter. There was also a slow telemetry mode for the cruise mode. The comet-encounter science data-take was from 2.5 h before until 0.5 h after the closest approach, with several periods of data-take before and after, each lasting about 2 h. Continuous coverage for plasma and dust instruments was provided by an onboard memory (5-megabit tape recorder). The spacecraft was shielded from hypervelocity dust impacts by a shield consisting of a 100-micrometer multilayer sheet 20 to 30 cm from the spacecraft, and a 1-mm Al sheet 5 to 10 cm from the spacecraft. Approximately half of the VEGA spacecraft was devoted to the Halley module, and half to the Venus lander package. The total scientific payload weight was 144.3 kg.
The Venus package consisted of a sphere 240 cm in diameter, which separated two days before arrival at Venus and entered the planet's atmosphere on an inclined path, without active maneuvers, as was done on previous Venera missions. The lander probe was identical to those of Venera 9 through 14 and similarly had two objectives, the study of the atmosphere and the study of the superficial crust. In addition to temperature and pressure measuring instruments, the descent probe carried a UV spectrometer for measurement of minor atmospheric constituents, an instrument dedicated to measurement of the concentration of H2O, and other instruments for determination of the chemical composition of the condensed phase: a gas-phase chromatograph; an X-ray spectrometer observing the fluorescence of grains or drops; and a mass spectrograph measuring the chemical composition of the grains or drops. The X-ray spectrometer separated the grains according to their sizes using a laser imaging device, while the mass spectrograph separated them according to their sizes using an aerodynamical inertial separator. After landing, a small surface sample near the probe was to be analyzed by gamma spectroscopy and X-ray fluorescence. The UV spectrometer, the mass spectrograph, and the pressure- and temperature-measuring instruments were developed in cooperation between French and Soviet investigators.
In addition to the lander probe, a constant-pressure instrumented balloon aerostat was deployed after entry into the atmosphere from the upper heat protection hemisphere. It floated at approximately 50 km altitude in the middle, most active layer of the Venus three-tiered cloud system. Data from the balloon instruments were transmitted directly to Earth for the 47-hr lifetime of the mission.
Information about the Vega 2 mission.
Soviet Academy of Sciences (U.S.S.R)
| Role | Person | |
|---|---|---|
| 1. | General contact | Mr. Artem Ivankov |
| 2. | Metadata contact | Jan Merka |
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National Space Science Data Center
| Role | Person | |
|---|---|---|
| 1. | General contact | Dr. Edwin J. Grayzeck, Jr. |
| 2. | General contact | Dr. Edwin V. Bell, II |