Image of the WIND Satellite(298 K)
About WIND:
This spacecraft is the first of NASA's
Global
Geospace Science (GGS) program, which is part of the
International
Solar-Terrestrial Physics (ISTP) Science Initiative, a
collaboration between several countries in Europe, Asia, and North
America. The aim of ISTP is to understand the behavior of
the solar-terrestrial plasma environment in order to predict how the Earth's
atmosphere will respond to changes in solar wind conditions. WIND's
objective is to measure the properties of the solar wind before it
reaches the Earth.
Schematic of WIND's instrumentation.
(14 K)
A more detailed
description of WIND is available from ISTP.
About the 3-D Plasma Instruments:
The U.W. Space Physics group is involved with the
3-D particle detectors that will provide unpredecented time resolution of
particle distributions in the solar wind and the magnetosphere.
Extensive documentation is available at the
3-D Plasma
and Energetic Particle Investigation Home Page, at the
U.C. Berkeley Space Science Laboratory.
Real-Time
Data and
Weekly
Status Reports are also available.
(The following is lifted verbatim from ISTP's
Spacecraft and Instruments Summary, which gives descriptions of
numerous ISTP instruments.)
Experiment Overview
The 3-D Plasma and Energetic Particle Analyzer investigation will measure ions
and electrons in the interplanetary medium with energies including that of the
solar wind and the energetic particle range.
It will study the particles upstream of the bow shock in the foreshock region
and the transient particles emitted by the Sun during solar particle events
following solar flares.
This experiment will cover the gap between the energy ranges covered by
SWE and
EPACT.
Science Objectives
To explore the interplanetary particle population in the thermal and
suprathermal energy range, to study the particle acceleration at the Sun, in
the interplanetary medium, and upstream from the Earth, to study transport of
particles and basic plasma processes in the interplanetary medium, and to
measure the particle and plasma input to and output from the Earth's
magnetosphere.
Measurement Objectives
To obtain the following measurements:
- The three dimensional distribution of plasma and energetic electrons
and ions over the particle energy range from solar wind to cosmic ray
energies, a few eV to several MeV.
- Energy resolution of 0.20 (deltaE/E) and angular resolution from 3 eV
to 30 keV; and energy resolution of 0.3 (deltaE/E) and angular
resolution of 22.5 degrees X 36 degrees, for particles from 20 keV to
11 MeV.
- Perturbations to the electron distribution function, in wave-particle
interactions.
Description of Instrument
The 3-D PLASMA instrument consists of two sensor packages mounted on
small radial booms, and an electronics package mounted inside the
spacecraft. One boom-mounted sensor package contains an array of 6
double-ended semiconductor telescopes, each with two or three closely
sandwiched silicon detectors to measure ebctrons and ions above 20
keV. One side of each telescope is covered with a thin foil which
absorbs ions below 400 keV. On the other side, the incoming electrons
below 400 keV are swept away by a magnet so that electrons and ions
are cleanly separated. Higher energy electrons (up to ~1 MeV) and
ions (up to 11 MeV) are identified by the two double-ended telescopes
which have a third detector. The first sensor package also contains a
pair of ion electrostatic analyzers (PESA-L and -H) for measuring ion
fluxes from ~3 eV to 40 keV. The second sensor package contains a
pair of electron electrostatic analyzers (EESA-L and -H) for measuring
electron fluxes from ~3 eV to 30 keV, and for making input (from
EESA-H) to a fast particle correlator (FPC). The FPC, using also
plasma wave data from WAVES as input, measures perturbations to the
electron distribution function and studies other wave-particle
interactions.
Who's Doing It:
- At the University of Washington
- Collaborators
- R.P. Lin, Principal Investigator, (U.C. Berkeley)
- C.W. Carlson (U.C. Berkeley)
- R. Ergun (U.C. Berkeley)
- J. McFadden (U.C. Berkeley)
- D. Larson (U.C. Berkeley)
- H. Reme (C.E.S.R., Toulouse, France)
- J.M. Bosqued (C.E.S.R., Toulouse, France)
- T. Sanderson (E.S.T.E.C., Noordwijk, The Netherlands)
- P.K. Wenzel (E.S.T.E.C., Noordwijk, The Netherlands)
- G. Paschmann (Max Planck, Garching, Germany)
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The WIND Spacecraft Experiment / 5 April 1995 /
freeman@geophys.washington.edu