This page summarizes information about the selected resource and its origin based on SPASE metadata.
SPASE version 2.0.0
High resolution (1m, 5m), multi-source, near-Earth solar wind magnetic field and plasma data as shifted to Earth's bow shock nose.
Extensive OMNI documentation pages
We acknowledge the experiment teams that acquired, processed and provided the OMNI-included data, and J.H. King and N.E. Papitashvili of NASA/GSFC for creating the OMNI data set.
| Role | Person | |
|---|---|---|
| 1. | General contact | Dr. Joseph H. King |
| 2. | Technical contact | Dr. Natalia E. Papitashvili |
Pathway to data and to extensive documentation. Plots, listings and user-specified files. Scatter plots and linear regressions. Distributions. Means, medians, standard deviations in distributions.
ftp access to monthly ASCII files of 1-min (10 MB/file) data and to annual ASCII files of 1-min (126 MB/file) and 5-min (25 MB/file) data.
We acknowledge the experiment teams that acquired, processed and provided the OMNI-included data, and J.H. King and N.E. Papitashvili of NASA/GSFC for creating the OMNI data set.
Various parameters are held current to differing levels. Typical delay is about 1-2 months.
Year.
Decimal day of year (Jan 1 = Day 1).
Decimal hour of day
Minute, start of the averaged interval
ID for magnetic field data source spacecraft for this 3-hour interval. See documentation cited above.
The following spacecraft IDs are used:
| ACE | 71 |
| Geotail | 60 |
| IMP 8 | 50 |
| Wind | 51 |
ID for plasma data source spacecraft for this 3-hour interval. See documentation cited above.
The following spacecraft IDs are used:
| ACE | 71 |
| Geotail | 60 |
| IMP 8 | 50 |
| Wind | 51 |
Number of fine scale points in magnetic field parameter averages for this minute
Number of fine scale points in plasma parameter averages for this minute
The percentage (0-100) of the points contributing to the 1-min magnetic field averages whose phase front normal (PFN) was interpolated because neither the MVAB-0 nor Cross Product shift techniques yielded a PFN that satisfied its respective tests (see detailed documentation for these).
Average time shift for all 15-s IMF values shifting into this minute.
Standard deviation in time shift average of previous word.
Standard deviation in phase front normal as averaged component-wise over the phase front normals determined for each 15-s IMF vector shifting into this minute.
Note that standard deviations for the two vectors are given as the square roots of the sum of squares of the standard deviations in the component averages. The component averages are given in the records but not their individual standard deviations.
Difference between mean observation time of IMF data shifting into this minute and into preceding minute. Negative values suggest "out of sequence" BSN arrivals.
Average of fine scale field magnitudes
Averaged GSE Cartesian components of magnetic field vector
Three 1-minute averaged magnetic field Cartesian components, in GSE
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | Bx, GSE | I | Column 15 |
| 2 | By, GSE | J | Column 16 |
| 3 | Bz, GSE | K | Column 17 |
Averaged GSM Cartesian components of magnetic field vector
Note that Bx(GSM)=Bx(GSE) is given only once in data record.
The GSM components are determined from post-shift GSE components.
Three 1-minute averaged magnetic field Cartesian components, in GSM
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | Bx, GSM | I | Column 15 |
| 2 | By, GSM | J | Column 18 |
| 3 | Bz, GSM | K | Column 19 |
Standard derviation in average of fine scale field magnitudes
Standard deviation of vector-averaged magnetic field vector. SQRT(sigma<Bx>**2 + sigma<By>**2 + Sigma<Bz>**2)
Note that standard deviations for the two vectors are given as the square roots of the sum of squares of the standard deviations in the component averages. The component averages are given in the records but not their individual standard deviations.
Plasma proton flow speed, variously derived for various OMNI-input data sets.
Averaged GSE Cartesian components of plasma velocity vector
Three 1-minute averaged plasma flow velocity Cartesian components, in GSE
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | Vx, GSE | I | Column 23 |
| 2 | Vy, GSE | J | Column 24 |
| 3 | Vz, GSE | K | Column 25 |
Plasma proton density, variously derived for various OMNI-input data sets. Cross normalized
Plasma proton temperature, variously derived for various OMNI-input data sets. Cross normalized
P (nPa) = (1.67/10**6) * Np*V**2 * (1+ 4*Na/Np), created from 1-min averaged Np, Na, V
-V(km/s) * Bz (nT; GSM) * 10**-3; Minute-averaged V and Bz used; nearly Ey component
[(T*4.16/10**5) + 5.34] * Np / B**2
(V * Np**0.5) / 20 * B
GSE Cartesian components of location of spacecraft providing IMF data
Three spacecraft location Cartesian components, in GSE
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | Rx, GSE | I | Column 32 |
| 2 | Ry, GSE | J | Column 33 |
| 3 | Rz, GSE | K | Column 34 |
GSE Cartesian components of location of Earth's bow shock nose (BSN), to which data have been shifted. Dynamically computed from solar wind parameters.
Three bow shock nose location Cartesian components, in GSE
| Index | Name | Component | Parameter key |
|---|---|---|---|
| 1 | BSNx, GSE | I | Column 35 |
| 2 | BSNy, GSE | J | Column 36 |
| 3 | BSNz, GSE | K | Column 37 |
SPASE version 2.0.0
The ACE Magnetometer (MAG) experiment consists of two triaxial fluxgate magnetometers mounted remotely on booms extending beyond the spacecraft solar panels at four meters from the spacecraft center. Each identical sensor (M1, M2) has a wide dynamic range of sensitivity at +- 0.004 to +- 65536 nT and measures the three vector components of the magnetic field. Usage of twin magnetometer sensors for measurements of weak interplanetary magnetic fields is a proven approach based on experience from many past space missions. The MAG sensors were originally built as spares for the MFI instrument on the WIND spacecraft and have been given minor modifications for inclusion on ACE. Readout of MAG data includes three data types: (1) average magnetic field vectors from the primary and secondary sensors, (2) "Snap-Shot Memory" data, and (3) Fast Fourier Transform (FFT) data. The average vector readout includes 216 bps corresponding to six vectors per second. These vector readouts can be split between M1 and M2 in the ratios of 3:3, 5:1, or 6:0. The "Snap-Shot Memory" stores field vectors at the maximum sampling rate of 30 vectors per second and is read out at 48 bps. The FFT readout includes 17 seconds accumulation of vector data transformed into spectral matrices of the components and total magnitude at a transmission rate of 32 bps. Prof. Norman F. Ness of the Bartol Research Institute at the University of Delaware is the MAG Experiment Manager.
Description of the ACE magnetometer design and instrument characteristics, with links to data and other documentation
Information about the Magnetometer (MAG) experiment on the ACE mission.
| Role | Person | |
|---|---|---|
| 1. | CoInvestigator | Dr. Norman F. Ness |
| 2. | Technical contact | Dr Charles W. Smith |
SPASE version 2.0.0
The Solar Wind Electron, Proton, and Alpha Monitor (SWEPAM) instrument sensors measure solar wind electrons at 1 - 900 eV energy and ions at 0.26 - 35 keV. The instrument consists of separate electron and ion analyzers originally built as spares for the Ulysses mission. The two sensors both utilizes curved-plate electrostatic analyzers (ESAs) consisting of spherical sections cut into sectors. Biased channel electron multipliers (CEMS) are spaced along the exit apertures of the ESAs for ion and electron detection. Different CEMs sample different portions of the fan-shaped fields of view. The ion sensor consists of a 105-degree bending angle ESA with an average radius of 100 mm and a plate spacing of 2.84 mm. Sixteen CEMs contiguously spaced along the exit gap of the ESA give about 5-degree polar angular resolution over the approximately 70-degree opening angle of the acceptance fan. The electron sensor consists of a 120-degree bending angle ESA with an average radius of 41.9 mm and a plate spacing of 3.5 mm. Seven large-funnel CEMs along the exit gap give about 20-degree angular resolution over a 160-degree fan angle. The sensor geometric factors are 0.002 cm2-sr for isotropic response and 0.009 cm2 for unidirectional. Energy resolution is five percent for ions and twelve percent for electrons. SWEPAM data consists of ion and electron rates collected at each energy/charge (E/Q) step, polar lock direction, and azimuthal spin direction. A single spacecraft spin period of 12 seconds is sufficient for accumulation of count matricies to fully calculate the electron and ion distribution functions from which bulk moments (solar wind speed, density, temperature) can be calculated by ground data processing. Accumulated counts will actually be summed over one-minute intervals for increased statistical accuracy and for reduction of telemetry requirements. Limited data from single spins will be provided for timing of the passage of transient solar wind structures.
Information about the SWEPAM instrument, with links to data and other documentation
Information about the Solar Wind Electron, Proton and Alpha Monitor (SWEPAM) experiment on the ACE mission.
| Role | Person | |
|---|---|---|
| 1. | CoInvestigator | Dr. David J. McComas |
| 2. | Technical contact | Ruth Skoug |
SPASE version 2.0.0
The magnetic field experiment on WIND provides data for studies of a broad range of scales of structures and fluctuation characteristics of the interplanetary magnetic field throughout the mission, and, where appropriate, relate them to the statics and dynamics of the magnetosphere. The basic instrument of the Magnetic Field Investigation (MFI) on the WIND Spacecraft is a boom-mounted dual triaxial fluxgate magnetometer and associated electronics. The dual configuration provides redudancy and also permits accurate removal of the dipolar portion of the spacecraft magnetic field. The instrument provides:
(1) near real-time data at nominally one vector per 92 s as key paramter data for broad dissemination, (2) rapid data at 10.9 vectors/s for standard analysis, (3) occasionally, snapshot (SS) memory data and Fast Fourier Transform data (FFT), both based on 44 vectors/s.
These measurements are precise (0.025%), accurate, ultra-sensitive (0.008 nT/step quantization), and where the sensor noise level is <0.006 nT r.m.s for 0-10 Hz. The digital processing unit utilizes a 12-bit microprocessor controlled analogue-to-digital converter. The instrument features a very wide dynamic range of measurement capability, from 4 nT up to 65 536 nT per axis in eight discrete ranges. (The upper range permits complete testing in the Earth's field.) In the FFT mode power spectral density elements are transmitted to the ground as fast as once every 23 s (high rate), and 2.7 min of SS memory time series data, triggered automatically by pre-set command, requires typically about 5.1 hours for transmission. Standard data products are the following vector field averages: 0.0226 s (detail data from SS), 0.092 s ('detail' in standard mode), 3 s, 1 min, and 1 hour, in both GSE and GSM coordinates, as well as the FFT spectral elements. High instrument reliability is obtained by the use of fully redundant systems and extremely conservative designs.
The instrument was turned on on 1994-11-12.
References: Lepping, R. P., et al., The WIND Magnetic Field Investigation, Space Science Reviews, 71, 207-229, 1995.
A web site hosting WIND MFI instrument information as well as web utilities for plotting and downloading data
User will acknowledge the WIND MFI instrument team in any publication resulting from the use of these data.
| Role | Person | |
|---|---|---|
| 1. | Data producer | Dr. Adam Szabo |
| 2. | Principal investigator | Dr. Ronald P. Lepping |
SPASE version 2.0.0
This investigation is designed to provide complete, accurate specification of solar wind flow parameters in real time. The instrument is a six-axis ion-electron spectrometer which provides three-dimensional velocity distribution functions for ions and electrons, with high time resolution. The energy range covered extends from 7 eV to 30 keV for electrons in four different modes, and from 30 eV to 30 keV in four different ion modes. In addition, two Faraday cups are used to obtain three-dimensional measurements of ions in 15-s periods, in the energy range 5 eV to 5 keV.
Information about the Solar Wind Experiment (SWE) experiment on the Wind mission.
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Dr. Keith W. Ogilvie |
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The magnetic field experiment on the IMP-8 spacecraft utilizes a tri-axial fluxgate (saturable inductor) magnetometer. The instrument originally had three, automatically determined, ranges, ±12 nT, ±36 nT, and ±108 nT, full scale. Because of a range-change circuit failure occurring in early July 1975, the experiment was commanded into a fixed ±36 nT range on July 11, 1975 at 12:55:09 UT and has been in that range ever since. The measurements are A-to-D converted onboard, to an 8-bit resolution, yielding ±0.14 nT quantization sensitivity, which is larger than the intrinsic sensor noise level of 0.025 nT RMS. The data from the two-bit (per component) adaptive delta modulator, incorporated into the instrument, and applied to the intrinsic sample rate of 25 vectors/sec., was never utilized, and hence the rate of the full (8-bit) vector words, which occur every 320 ms, represents the effective sample period of the instrument. The sampling rate is synchronized to the spacecraft clock; the basic spacecraft clock frequency is 6.4 kHz. The sensor unit is mounted on the end of a boom approximately 4 m from the center of the spacecraft.
A web site hosting IMP-8 magnetic experiment instrument information as well as web utilities for plotting and downloading data.
Information about the Magnetic Field Experiment experiment on the IMP 8 mission.
User will acknowledge the IMP-8 magnetometer team in any publication resulting from the use of these data.
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Dr. Adam Szabo |
SPASE version 2.0.0
A modulated split-collector Faraday cup, perpendicular to the spacecraft spin axis, was used to study the directional intensity of positive ions and electrons in the solar wind, transition region, and magnetotail. The collector plate split is perpendicular to the spacecraft spin axis in order to measure the flow angle of the ions in a meridional plane; the flow angle in the spacecraft equatorial plane is determined from the fluxes measured as the spacecraft rotates.
Electrons are measured using 21 logarithmically-spaced energy windows covering the energy/charge range between 23 and 1935 volts. Positive ions are studied using 24 energy windows covering the range between 50 and 7000 volts.
The instrument has three operating modes. The tracking mode yields the best time resolution which is about 1 minute. A single energy window is used during a spacecraft rotation. The ion spectrum is obtained in eight spacecraft revolutions using a subset of the energy windows that track the peak of the solar wind. In this mode, fluxes are measured during 11.25-degree sectors of the spacecraft spin while the instrument is looking within the 90 degree sector centered on the sun direction and during 45 degree sectors for the remainder of the rotation. The other modes yield a spectrum using all 24 windows (with the same angular sectors described above) or a spectrum that results from integrating the observed fluxes over 45 degree sectors for the entire spacecraft rotation.
Electron data are obtained in all modes, but are not usually analyzed.
Parameters derived on a routine basis are proton velocity, number density, and temperature (most probable thermal speed). Those parameters are obtained from a non-linear, least-squares fit to the observed fluxes using a convected, isotropic Maxwellian model.
Key Parameters for the Plasma instrument are computed at MIT using Level Zero data that are staged to the ISTP/CDHF approximately two weeks after being received on Earth. Thus the plasma instrument's Key Parameters lag real time by something greater than 2 weeks, but less than four.
Information about the Solar Plasma Faraday Cup experiment on the IMP-J mission.
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Dr. Alan J. Lazarus |
SPASE version 2.0.0
The objective of this experiment is to measure the magnetic field variation of the magnetotail in the frequency below 50 Hz. The MGF experiment consists of dual three-axis fluxgate magnetometers and a three-axis search coil magnetometer. Triad fluxgate sensors, which utilize a ring core geometry, are installed at the end and middle of a 6 m deployable mast. Three search coils are mounted approximately one-half of the way out on another 6 m boom together with search coils for the VLF wave in the PWI system.
The fluxgate magnetometers are of standard design and consist of an amplifier, filter, phase sensitive detector, integrator, and a voltage-current convertor. The fluxgate magnetometers operate in seven dynamic ranges to cover various regions of the Earth's magnetosphere and the solar wind: +/-16 nT, +/-64 nT, +/-256 nT, +/-1024 nT, +/-4096 nT, +/-16384 nT, and +/-65536 nT, and supply 16 vectors/sec.
The automatic range control of the fluxgate magnetometers failed in 1999 so the observable range was manually fixed in the +/-256 nT where it has remained ever since. On November 23, 2006, the fluxgate magnetometer at the end of the boom failed and data from the second magnetometer at the middle of the boom has been used ever since. Neither of the above changes substantially affect the data.
The search coil magnetometer system consists of three sensors, preamplifier, amplifier, filter, multiplexer, and an A/D converter. The search coil magnetometers operate in a frequency range of 0.5 kHz to 1 kHz, and supply 128 vectors/sec. The fluxgate magnetometer operates in both real time and record modes, while the search coil data are used only in real time mode.
Information about the Magnetic Fields Measurement (MGF)
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Prof. Tsugunobu Nagai |
| 2. | Scientist | Dr. Donald H. Fairfield |
| 3. | Metadata contact | Jan Merka |
SPASE version 2.0.0
The objective of the Comprehensive Plasma Instrumentation (CPI) investigation is to make comprehensive observations of the three-dimensional velocity distribution functions of electrons and positive ions, with identification of ion species. The instrument contains three sets of quadrispherical analyzers with channel electron multipliers. These three obtain three-dimensional measurements for hot plasma and solar wind electrons, for solar wind ions, and for positive-ion composition measurements. The positive-ion composition measurement of the Ion Composition (IC) analyzer includes five miniature imaging mass spectrometers at the exit aperture of the analyzer, and covers masses from 1 to 550 u/Q at 100 eV, and 1 to 55 u/Q at 10 keV. The Hot Plasma (HP) analyzer measures electrons and ions in the range 1-50,000 eV/Q. The Solar Wind (SW) analyzer measures ions from 150 to 7,000 eV/Q. Sequencing of the energy analyzers and mass spectrometers, and other control functions, are provided by two microprocessors.
Information about the Comprehensive Plasma Instrument (CPI)
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Prof. Louis A. Frank |
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The objective of the Advanced Composition Explorer (ACE) is to collect observations of particles of solar, interplanetary, interstellar, and galactic origins, spanning the energy range from that of KeV solar wind ions to galactic cosmic ray nuclei up to 600 MeV/nucleon. Definitive studies will be made of the abundances of essentially all isotopes from H to Zn (Z = 1-30), with exploratory isotope studies extending to Zr (Z = 40). The ACE payload includes six high resolution spectrometers, each designed to provide the optimum charge, mass, or charge-state resolution in its particular energy range. Each spectrometer has a geometry factor optimized for the expected flux levels, so as to provide a collecting power greater by a factor of 10-1000 times that of previous or planned experiments. The payload also includes three additional instruments of standard design to monitor energetic electrons, H and He ions, and a magnetometer. The ACE spacecraft is based on the design of the Charge Composition Explorer, built at JHU/APL for the Active Magnetospheric Particle Tracer Explorer (AMPTE) program. The spacecraft spin axis is pointed towards the Sun to within +/- 20 degrees, and it occupies a halo orbit about the L1 Earth-Sun libration point. Powered by solar cells, the spacecraft has a design life of at least five years, and it returns data in daily tape recorder dumps, received through NASA JPL's Deep Space Network and initially processed at NASA-GSFC. The average data telemetry rate is 6.7 Kbs.
ACE mission home page at Caltech with data download
Information about the ACE mission
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Prof. Edward C. Stone, Jr. |
SPASE version 2.0.0
The Wind spacecraft was launched on November 1, 1994 and is the first of two NASA spacecraft in the Global Geospace Science initiative and part of the ISTP Project. The science objectives of the WIND mission are: (1) Provide complete plasma, energetic particle, and magnetic field input for magnetospheric and ionospheric studies; (2) Determine the magnetospheric output to interplanetary space in the up-stream region; (3) Investigate basic plasma processes occurring in the near-Earth solar wind; and (4) Provide baseline ecliptic plane observations to be used in heliospheric latitudes from ULYSSES.
Wind has on-board propulsion and its design lifetime is three to five years, with redundant subsystems. Wind is cylindrical, approximately 2.8 m in diameter by 1.25 m high, with body-mounted solar cells. It has long wire spin-plane antennas, inertial booms, and spin-plane appendages to support sensors. Wind has experiment booms deployed along both Z axes. The spin rate is 20 rpm around an axis within 1 degree of normal to the ecliptic.
Data are stored using on-board tape recorders and are relayed to the Deep Space Network at one of two rates: 5.5 or 11.1 kbps.
For the first nine months of operation, Wind was placed in a double-lunar swingby orbit near the ecliptic plane, with apogee from 80 to 250 Earth radii and perigee of between 5 and 10 Earth radii. In this orbit, lunar gravity assists were used to keep its apogee over the day hemisphere of the Earth, and magnetospheric observations are made. Wind was then inserted into a small "halo" orbit, about the sunward Sun-Earth gravitational equilibrium point (L1), varying from 235 to 265 Earth radii. In this orbit Wind measures the incoming solar wind, magnetic fields and particles continuously and provides an approximately one-hour warning to the other ISTP spacecraft of changes in the solar wind.
In 2001 and 2002 Wind has executed a distant prograde orbit that took it +/- 300 Re leading and legging Earth. This orbit provided a wide baseline to study solar wind structures and correlations. In 2003, Wind reached the L2 Lagrange point 240 Re anti-sunward from Earth providing a 500 Re spatial separation from ACE solar wind observations along with measurements of the distant Earth magnetotail. Since 2004, Wind has been permanently parked in a L1 halo orbit where it continues to provide high-quality solar wind measurements.
Information about the Wind mission
| Role | Person | |
|---|---|---|
| 1. | Project scientist | Dr. Adam Szabo |
SPASE version 2.0.0
IMP 8 (IMP-J or Explorer 50), the last satellite of the IMP series, was a drum-shaped spacecraft, 135.6 cm across and 157.4 cm high, instrumented for interplanetary and magnetotail studies of cosmic rays, energetic solar particles, plasma, and electric and magnetic fields. Its initial orbit was more elliptical than intended, with apogee and perigee distances of about 45 and 25 earth radii. Its eccentricity decreased after launch. Its orbital inclination varied between 0 deg and about 55 deg with a periodicity of several years. The spacecraft spin axis was normal to the ecliptic plane, and the spin rate was 23 rpm. The data telemetry rate was 1600 bps.
The spacecraft was in the solar wind for 7 to 8 days of every 12.5 day orbit. Telemetry coverage was 90% in the early years, but only 60-70% through most of the 1980's and early 1990's. Coverage returned to the 90% range in the mid to late 1990's.
The objectives of the extended IMP-8 operations were to provide solar wind parameters as input for magnetospheric studies and as a 1-AU baseline for deep space studies, and to continue solar cycle variation studies with a single set of well-calibrated and understood instruments.
In October, 2001, IMP 8 was terminated as an independent mission. Telemetry acquisition resumed after about three months at Canberra only (30-50% coverage), as an adjunct to the Voyager and Ulysses missions. As of August 2005 IMP 8 continued in this mode.
Information about the IMP-J mission
| Role | Person | |
|---|---|---|
| 1. | Project scientist | Dr. Robert E. McGuire |
SPASE version 2.0.0
The solar wind draws the Earth's magnetic field into a long tail on the nightside of the Earth and stores energy in the stretched field lines of the magnetotail. During active periods, the tail couples with the near-Earth magnetosphere, sometimes releasing energy stored in the tail and activating auroras in the polar ionosphere.
The Geotail mission measures global energy flow and transformation in the magnetotail to increase understanding of fundamental magnetospheric processes. This includes the physics of the magnetopause magnetospheric boundary regions, the lobe and plasma sheet, and reconnection and neutral line formation, i.e., the mechanisms processes of input, transport, storage, release and conversion of mass, momentum and energy in the magnetotail.
Geotail, together with Wind, Polar, SOHO, and Cluster projects, constitute a cooperative scientific satellite project designated the International Solar Terrestrial Physics (ISTP) program which aims at gaining improved understanding of the physics of solar-terrestrial relations.
Geotail is a spin-stabilized spacecraft utilizing mechanically despun antennas with a design lifetime of about four years. The nominal spin rate of the spacecraft is about 20 rpm around a spin axis maintained between 85-89 degrees to the ecliptic plane. Geotail is cylindrical, approximately 2.2 m in diameter, and 1.6 m high. with It has body-mounted solar cells. Geotail also has and a back-up battery subsystem which that operates when the spacecraft is in the Earth's shadow (limited to 2 hrs). Real-time telemetry data transmitted in X-band are received at the Usuda Deep Space Center (UDSC) in Japan. There are two tape recorders on board, each with a capacity of 450 Mb, which allows daily 24-hour data coverage and are collected in playback mode by the NASA Deep Space Network (DSN).
The Geotail mission is divided into two phases. During the two-year initial phase, the orbit apogee was kept on the nightside of the Earth by using the Moon's gravity in a series of double-lunar swing-by maneuvers that result in the spacecraft spending most of its time in the distant magnetotail (maximum apogee about 200 Earth radii) with a period varying from one to four months. Then, in November 1994, there were a series of maneuvers that reduced the apogee to 50 Re. After three more months in the magnetotail the spacecraft was put in a 10 by 30 Re orbit where it has remained except that the perigee was reduced from 10 to 9 Re in June 1997.
Details on the Geotail mission and instrumentation are given in the Journal of Geomagnetism and Geoelectricity (Vol. 46, No. 1, 1994); online from JGG at
http://www.terrapub.co.jp/journals/EPS/JGG
Information about the Geotail mission
| Role | Person | |
|---|---|---|
| 1. | Project scientist | Guan Le |
| 2. | Project scientist | Prof. Masaki Fujimoto |
| 3. | Metadata contact | Jan Merka |
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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 |