This page summarizes information about the selected resource and its origin based on SPASE metadata.
SPASE version 2.0.0
12-second Editor-A low-energy particle data from the Geotail spacecraft.
Editor-A data are only acquired with the real-time operation in Usuda Deep Space Center (UDSC),Japan, while the Editor-B data are 24-hours continuouslyrecorded in the onboard tape recorders and are dumpedover the NASA/JPL Deep Space Network (DSN) stations.
The ion energy analyzer (LEP-EAi) has two energy scan mode: RAM-A (60 eV to 40 keV) and RAM-B (5 keV to 40 keV). RAM-B is selected to protect the very sensitive detector from intense low energy fluxes that are usually seen in the solar wind and magnetosheath. The energy scan mode is automatically selected onboard depending on incoming ion fluxes. At present, only the ion moments in the RAM-A mode are listed for the LEP-EAi data.
The ion moment data of the solar wind analyzer (LEP-SW) should be used only qualitatively. The LEP-SW ion moments are listed when the energy scan mode of LEP-EAi is RAM-B.
Reprint of Mukai, T., S. Machida, Y. Saito, M. Hirahara, T. Terasawa, N. Kaya, T. Obara, M. Ejiri, and A. Nishida, The low energy particle (LEP) experiment onboard the Geotail satellite, J. Geomag. Geoelectr., 46, 669-692, 1994.
In any publications, the use of the Geotail data should be acknowledged, for example, as "Geotail magnetic field data were provided by Y. Saito, JAXA in Japan."
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Dr. Yoshifumi Saito |
| 2. | Scientist | Dr. Donald H. Fairfield |
| 3. | Metadata contact | Jan Merka |
Data provider Y. Saito at JAXA, Japan and CDAWeb.
Data ARchives and Transmission System (DARTS) is a versatile space science data archive for astrophysics, solar physics, and solar-terrestrial physics. DARTS primarily consists of the data acquired by Japanese scientific satellites and spacecrafts. DARTS is developed and maintained by the Center of Science-satellite Operation and Data Archive (C-SODA) at ISAS/JAXA.
In any publications, the use of the Geotail data should be acknowledged, for example, as "Geotail magnetic field data were provided by Y. Saito through DARTS at Institute of Space and Astronautical Science, JAXA in Japan."
Please use the Editor-A LEP dataset prior to the Editor-B LEP dataset since plasma moments in the Editor-A data are more reliable. (Plasma moments inthe Editor-B are calculated onboard.)
The ion moment data of the solar wind analyzer (LEP-SW) should be used only qualitatively.
Number of milliseconds since the CDF epoch
Ion density
Qualitative use only if Energy Scan Code = 2, i.e. if the energy scan mode is RAM-B/SW.
Ion temperature in satellite coordinates
Qualitative use only if Energy Scan Code = 2, i.e. if the energy scan mode is RAM-B/SW.
| Index | Name | Valid min | Valid max | Fill value |
|---|---|---|---|---|
| 1 | Ti,yy | -10 | 10000 | -1.0E31 |
| 2 | Ti,zz | -10 | 10000 | -1.0E31 |
Name of the instrument sensor measuring data.
Energy scan code/mode:
Ion velocity in GSE coordinates
Qualitative use only if Energy Scan Code = 2, i.e. if the energy scan mode is RAM-B/SW.
| Index | Name | Component | Valid min | Valid max | Fill value |
|---|---|---|---|---|---|
| 1 | Vxi (GSE) | I | -2000 | 2000 | -1.0E31 |
| 2 | Vyi (GSE) | J | -2000 | 2000 | -1.0E31 |
| 3 | Vzi (GSE) | K | -2000 | 2000 | -1.0E31 |
Geotail position in GSE cartesian coordinates
1 Re = 6371.2 km
| Index | Name | Component | Valid min | Valid max | Fill value |
|---|---|---|---|---|---|
| 1 | X (GSE) | I | -500.0 | 500.0 | -1.0E31 |
| 2 | Y (GSE) | J | -500.0 | 500.0 | -1.0E31 |
| 3 | Z (GSE) | K | -500.0 | 500.0 | -1.0E31 |
Ion velocity in GSM coordinates
Qualitative use only if Energy Scan Code = 2, i.e. if the energy scan mode is RAM-B/SW.
| Index | Name | Component | Valid min | Valid max | Fill value |
|---|---|---|---|---|---|
| 1 | Vxi (GSM) | I | -2000 | 2000 | -1.0E31 |
| 2 | Vyi (GSM) | J | -2000 | 2000 | -1.0E31 |
| 3 | Vzi (GSM) | K | -2000 | 2000 | -1.0E31 |
Geotail position in GSM cartesian coordinates
1 Re = 6371.2 km
| Index | Name | Component | Valid min | Valid max | Fill value |
|---|---|---|---|---|---|
| 1 | X (GSM) | I | -500.0 | 500.0 | -1.0E31 |
| 2 | Y (GSM) | J | -500.0 | 500.0 | -1.0E31 |
| 3 | Z (GSM) | K | -500.0 | 500.0 | -1.0E31 |
Ion velocity in SM coordinates
Qualitative use only if Energy Scan Code = 2, i.e. if the energy scan mode is RAM-B/SW.
| Index | Name | Component | Valid min | Valid max | Fill value |
|---|---|---|---|---|---|
| 1 | Vxi (SM) | I | -2000 | 2000 | -1.0E31 |
| 2 | Vyi (SM) | J | -2000 | 2000 | -1.0E31 |
| 3 | Vzi (SM) | K | -2000 | 2000 | -1.0E31 |
Geotail position in SM cartesian coordinates
1 Re = 6371.2 km
| Index | Name | Component | Valid min | Valid max | Fill value |
|---|---|---|---|---|---|
| 1 | X (SM) | I | -500.0 | 500.0 | -1.0E31 |
| 2 | Y (SM) | J | -500.0 | 500.0 | -1.0E31 |
| 3 | Z (SM) | K | -500.0 | 500.0 | -1.0E31 |
SPASE version 2.0.0
The low energy particle (LEP) instrument onboard Geotail is designed to make comprehensive observations of plasma and energetic electrons and ions with fine temporal resolution in the terrestrial magnetosphere (mainly magnetotail) and in the interplanetary medium. It consists of three units of sensors (LEP-EA, LEP-SW and LEP-MS) and common electronics (LEP-E).
The Energy-per-charge Analyzers (EA) measure three-dimensional velocity distributions of electrons (with EA-e) and ions (with EA-i) simultaneously and separately, over the energy-per-charge of several eV/q to 43 keV/q. Emphasis in the EA design is laid on the large geometrical factor to measure tenuous plasma in the magnetotail with sufficient counting statistics in the high-time-resolution measurement.
On the other hand, the Solar Wind ion analyzer (SW) has smaller geometrical factor, but fine angular and energy resolutions, to measrue energy-per-charge spectra of the solar wind ions. In both EA and SW sensors, the complete three-dimensional velocity distributions can only be obtained in a period of four spins, while the velocity moments up to the third order are calculated onboard every spin period (nominally, 3 sec).
The energetic-ion Mass Spectrometer (MS) failed shortly after launch and no data are available.
Reprint of Mukai, T., S. Machida, Y. Saito, M. Hirahara, T. Terasawa, N. Kaya, T. Obara, M. Ejiri, and A. Nishida, The low energy particle (LEP) experiment onboard the Geotail satellite, J. Geomag. Geoelectr., 46, 669-692, 1994.
In any publications, the use of the Geotail LEP data should be acknowledged, for example, as "Geotail magnetic field data were provided by Y. Saito, JAXA in Japan."
| Role | Person | |
|---|---|---|
| 1. | Principal investigator | Dr. Yoshifumi Saito |
| 2. | Scientist | Dr. Donald H. Fairfield |
| 3. | Metadata contact | Jan Merka |
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 |
SPASE version 2.0.0
SPASE version 2.0.0
SPASE version 2.0.0
SPASE version 2.0.0
SPASE version 2.0.0
SPASE version 2.0.0
SPASE version 1.2.0
Coordinated Data Analysis Web (CDAWeb) supports not only interactive plotting of variables from multiple instruments on multiple investigations simultaneously on arbitrary, user-defined time-scales. It also supports data retrieval in various formats using its interactive web interface or ftp service.
Coordinated Data Analysis Web (CDAWeb) home page at Space Physics Data Facility of the NASA Goddard Space Flight Center.
| Role | Person | |
|---|---|---|
| 1. | Project scientist | Dr. Robert E. McGuire |
SPASE version 1.3.4
Data ARchives and Transmission System (DARTS) is a versatile space science data archive for astrophysics, solar physics, and solar-terrestrial physics. DARTS primarily consists of the data acquired by Japanese scientific satellites and spacecrafts. DARTS is developed and maintained by the Center of Science-satellite Operation and Data Archive (C-SODA) at ISAS/JAXA.
DARTS front page.
| Role | Person | |
|---|---|---|
| 1. | Metadata contact | Jan Merka |