This page summarizes information about the selected resource and its origin based on SPASE metadata.
SPASE version 2.0.0
This is an hourly resolution, merged magnetic field and plasma data set created at NSSDC for COHOWeb. Magnetic field vectors and plasma flow direction angles are given in RTN coordinates. Spacecraft position data are given in Heliographic inertial (HGI coordinates).
Please acknowledge the magnetic field and plasma Principal Investigators, Drs. C.T. Russell and P. Gazis, and NSSDC or GSFC-SPDF
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Dr. Christopher T. Russell |
| 2. | Principal investigator | Dr. Paul R. Gazis |
| 3. | General contact | Dr. Natalia E. Papitashvili |
for annual files via ftp
Pioneer_Venus-specific page for plots and lists
Plots, lists, scatter plots, regressions, distributions, means, etc.
Please acknowledge the magnetic field and plasma Principal Investigators, Drs. C.T. Russell and P. Gazis, and NSSDC or GSFC-SPDF
Plasma data end on Oct. 9, 1992. Magnetic field data end on Aug. 7, 1988.
Four digit Year
Decimal Day of Year
Hour
Pioneer Venus location relative to the center of Venus, in Venus Solar Orbital coordinates (x from Venus to sun, z northward from Venus orbit plane)
The data set contains Venus-centered PVO location in Venus Solar Orbital coordinates. (X from Venus to sun, Z positive northward from Venus orbit plane). This coordinate system is presently not available in the data model. "SSE" (spacecraft solar ecliptic) is used as an approximation. Most if not all heliospheric studies for which hourly data are used, assuming the data were taken as the location of the center of Venus should be fine.
X,Y,Z components
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | X component | I | Column04 |
| 2 | Y component | J | Column05 |
| 3 | Z component | K | Column06 |
Heliocentric radial distance of Planet Venus in AU
Heliographic Inertial elevation angle of Planet Venus in deg
Heliographic Inertial azimuthal angle of Planet Venus in deg
Hourly averages of XYZ components of fine time scale magnetic field vectors. Coordinate System is Venus Solar Orbital (VSO)
X, Y, Z components in Venus Solar Orital (VSO) coordinates
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | X component | I | Column10 |
| 2 | Y component | J | Column11 |
| 3 | Z component | K | Column12 |
Hourly averages of RTN components of fine time scale magnetic field vectors
R,T,N components
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | R component | I | Column13 |
| 2 | T component | J | Column14 |
| 3 | N component | K | Column15 |
Hourly average of fine time scale magnetic field magnitudes
Hourly averaged solar wind plasma flow speed
Hourly averaged solar wind plasma flow elevation angle
Hourly averaged solar wind plasma flow azimuthal angle
Hourly averaged solar wind plasma density
Hourly averaged solar wind plasma temperature
SPASE version 2.0.0
This experiment used a triaxial fluxgate magnetometer with two ring-core sensors at the end of a magnetometer boom and one ring-core sensor, at 45 degrees to the spin axis, halfway down the boom. The drive and electronics design had been used on the Apollo 15 and 16 subsatellites. The objectives of this investigation were to: (1) determine any planetary and remnant magnetic fields; (2) deduce the location and strength of the ionospheric current system; (3) determine the energy and mass balance in the upper atmosphere of Venus; (4) examine the nature of the solar wind interaction with Venus; and, (5) study the near-wake region of Venus and the structure of the Venusian bow shock. Additional objectives for interplanetary (solar wind) studies were to determine the perturbation of the near-planet region by Venus and to compare the properties of the average field at 0.7 and 1.0 AU. The instrument was intended to, in the worst case of low-bit and low-sample rates, measure one vector per 32 s. While in Venus orbit, when the spacecraft was coasting through the interplanetary region in the apoapsis mode, the sample rate was one vector per 8 s. While the spacecraft was passing through Venus' ionosphere in the periapsis mode, the sample rate was four vectors per second. The last full orbit of three-axis data was 3602, which ended on 16 Oct. 1988 at 14:30 UT. After this time, only one-axis data were available.
Information about the Magnetometer (OMAG) experiment on the Pioneer Venus Orbiter mission.
| Role | Person | |
|---|---|---|
| 1. | General contact | Dr. Christopher T. Russell |
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This investigation used a Langmuir-probe retarding-potential analyzer designed to measure electron concentration and temperature, major ion concentrations and temperatures, ion drift velocities, and the energy distribution function of ambient photoelectrons. It was an adaptation of the instrument flown on the German Aeros satellite in 1972. Either one of two sensor heads could be used, each consisting of a multigrid cup and electrometer, which could operate in electron, ion, or photoelectron modes, initiated by spacecraft roll pulses. The measurements taken when the sensor axis was closest to the plasma flow velocity vector were transmitted. The aims of the investigation were to improve knowledge of the important ionic reactions in the Venusian ionosphere, to study the plasma transport processes to determine if Venus has a polar wind, to study the processes at the solar wind-ionosphere boundary, and to study similar aims concerning the ambient electron population.
Information about the Retarding Potential Analyzer (ORPA) experiment on the Pioneer Venus Orbiter mission.
| Role | Person | |
|---|---|---|
| 1. | General contact | Dr. William C. Knudsen |
SPASE version 2.0.0
The Pioneer Venus Orbiter was the first of a two-spacecraft orbiter-probe combination designed to conduct a comprehensive investigation of the atmosphere of Venus. The spacecraft was a solar-powered cylinder about 250 cm in diameter with its spin axis spin-stabilized perpendicular to the ecliptic plane. A high-gain antenna was mechanically despun to remain focused on the earth. The instruments were mounted on a shelf within the spacecraft except for a magnetometer mounted at the end of a boom to ensure against magnetic interference from the spacecraft. Pioneer Venus Orbiter measured the detailed structure of the upper atmosphere and ionosphere of Venus, investigated the interaction of the solar wind with the ionosphere and the magnetic field in the vicinity of Venus, determined the characteristics of the atmosphere and surface of Venus on a planetary scale, determined the planet's gravitational field harmonics from perturbations of the spacecraft orbit, and detected gamma-ray bursts. UV observations of comets have also been made. From Venus orbit insertion on December 4, 1978 to July 1980 periapsis was held between 142 and 253 km to facilitate radar and ionospheric measurements. Thereafter, the periapsis was allowed to rise (to 2290 km at maximum) and then fall, to conserve fuel. In 1991 the Radar Mapper was reactivated to investigate previously inaccessible southern portions of the planet. In May 1992 Pioneer Venus began the final phase of its mission, in which the periapsis was held between 150 and 250 km until the fuel ran out and atmospheric entry destroyed the spacecraft the following August. The orbiter cost $125 million to build and operate for the first 10 years. For further details see Colin, L. and Hunten, D. M., Space Science Reviews 20, 451, 1977.
Information about the Pioneer Venus Orbiter mission
| Role | Person | |
|---|---|---|
| 1. | Project scientist | Dr. Lawrence Colin |
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Space Physics Data Facility
Space Physics Data Facility
| Role | Person | |
|---|---|---|
| 1. | General contact | Ms. Tamara J. Kovalick |
| 2. | Technical contact | Mr. Robert M. Candey |
| 3. | Project scientist | Dr. Robert E. McGuire |