Data Set Information
|
DATA_SET_NAME |
MGS MARS/MOONS MAG/ER PRE-MAP ER OMNIDIRECTIONAL FLUX V1.0
|
DATA_SET_ID |
MGS-M-ER-3-PREMAP/OMNIDIR-FLUX-V1.0
|
NSSDC_DATA_SET_ID |
|
DATA_SET_TERSE_DESCRIPTION |
Calibrated time-ordered data tables from the
Electron Reflectometer instrument on the Mars Global Surveyor
spacecraft, collected during the premapping period of the mission.
|
DATA_SET_DESCRIPTION |
====================================================================
Data Set Overview
=================
The Electron Reflectometer Data Record (ERDR) is a time ordered
series of electron measurements from the Mars Global Surveyor (MGS)
Mission. Each record consists of a time tag with 19 scalar data
points representing measurements of the electron flux in 19
different energy channels, ranging from 10 eV to 20 keV, with an
energy resolution of 25%. Each data point is a measure of the
electron flux (cm-2 sec-1 ster-1 eV-1) averaged over a 360 x 14
degree disk-shaped field of view (FOV). (Parts of this FOV are
masked because of spacecraft obstructions, as described below.)
During the Science Phasing Orbits (SPO), the spacecraft was in
Array Normal Spin (ANS) configuration, for which the ER field of
view sweeps out the entire sky (4-pi ster) every 50 minutes, which
is much longer than the integration time per record (2 to 48 sec,
depending on energy and telemetry rate) and much longer than most
timescales of interest in Mars' plasma environment.
The ERDR is intended to be used in conjunction with MGS
Magnetometer (MAG) data records, which provide the magnetic field
vector and spacecraft ephemeris data as a function of time.
Electrons travel along the magnetic field lines in tight helices
(few km radius) at high speed (roughly one Mars diameter per
second). Thus the electron data contain information about the
plasma environment as well as the large-scale configuration of the
magnetic field, which is sampled locally by the MAG.
===================================================================
Parameters
==========
The Mars Global Surveyor ER data set consists of a time ordered
series of electron flux measurements in 19 energy channels, ranging
from 10 eV to 20 keV. The ER data are organized into ''packets,''
each of which contains 12, 24, or 48 seconds of data, respectively,
for high, medium, and low spacecraft telemetry rates. Each packet
is further subdivided into samples. There are from 1 to 6 samples
per packet, depending on the energy channel, as given in the table
below. The ER data set is generated at the rate of 6 samples per
packet, regardless of energy. When there are fewer than 6 samples
per packet at a particular energy, data values are repeated in
order to maintain a uniform table. The time listed for each record
is the center of the sampling interval. When records are repeated,
taking an average of the times for all repeated records provides
the center time for that sample.
The energy channels and sampling intervals are as follows:
Channel Number Energy Range Samples per Packet
---------------------------------------------------------------
0 13 - 20 keV 1
1 8.0 - 12 keV 1
2 4.9 - 7.5 keV 1
3 2.9 - 4.6 keV 3
4 1.8 - 2.8 keV 3
5 1.1 - 1.7 keV 3
6 680 - 1046 eV 6
7 415 - 639 eV 6
8 253 - 390 eV 6
9 153 - 237 eV 6
10 92 - 144 eV 6
11 72 - 87 eV 2
12 56 - 67 eV 2
13 43 - 52 eV 1
14 33 - 40 eV 2
15 25 - 30 eV 1
16 18 - 23 eV 2
17 14 - 17 eV 1
18 10 - 13 eV 2
---------------------------------------------------------------
The ER has a 360 x 14 degree disk-shaped field of view. The 360
degrees are divided into 16 angular sectors, each with a separate
counter that is read out in telemetry. The sizes and look
directions of these sectors are programmable to within an accuracy
of 1.4 degrees. The ER can operate in one of two modes: PAM-fixed
or PAM-variable. In PAM-variable mode, the sizes and look
directions of the 16 angular sectors are dynamically chosen by the
DPU (using onboard MAG data) in order to map the FOV into fixed
pitch angle bins. PAM-variable mode is used only in the mapping
orbit. Throughout the SPO period, the ER was in PAM-fixed mode,
meaning that the FOV was divided into 16 equally sized 22.5 x 14
degree sectors that remained fixed in spacecraft coordinates.
Some of these PAM-fixed sectors are masked because of obstructions
in the FOV, most notably the stowed high gain antenna (HGA), which
blocks 3 sectors. Three additional sectors are partially obstructed
by the -Y solar array gimbal/yoke assembly and corners of the
spacecraft bus. These obstructions are minimal, so data from these
sectors is still considered to be of good quality in PAM-fixed
mode. Finally, one sector was damaged in the interval between
SPO-1 and SPO-2, and its efficiency dropped by about a factor of 4.
For this SPO data set, the 3 sectors obstructed by the HGA and the
one damaged sector are masked, and we sum data from all other
sectors to form a scalar ''omnidirectional'' value. The effective
FOV for each record consists of two 135 x 14 degree fans.
====================================================================
Processing
==========
Processing is carried out at the Space Sciences Laboratory (SSL) of
the University of California, Berkeley, (UCB) to convert the raw
data to measurements of the omnidirectional electron flux (cm-2 s-1
ster-1 eV-1). Because of the instrument's high dynamic range (six
decades), the onboard digital processing unit (DPU) compresses the
raw counts in a logarithmic scale. The first step is to decompress
the raw counts and construct a three-dimensional data array, where
the first dimension is time (6 elements per telemetry packet), the
second dimension is direction around the FOV (16 elements), and the
third dimension is energy (19 elements).
The next step is to sum over unobstructed angular sectors to
produce a two-dimensional time/energy array. Raw count rate (R) is
then obtained by dividing the raw counts by the integration time
(0.0625 sec per energy step). The data are next corrected for
deadtime. During the time it takes the instrument to process a
single electron (known as the ''deadtime'', which is about 0.4
microsec for the ER), it ignores any other electrons. The raw
count rate is multiplied by the factor 1/(1 - RT), where T is the
deadtime, to obtain corrected count rate. Data values are masked
(set to -9.999e-9) when the deadtime correction factor exceeds
1.25. These data are NOT CORRECTED for a background count rate due
to cosmic rays and noise in the electronics (about 10 counts/sec).
Most of the time, the signal in the highest energy channel (13-20
keV) is dominated by background. Exceptions to this sometimes
occur during bowshock crossings or during energetic solar events.
Assuming that the highest energy channel contains 100% background,
the background level for the lower energy channels can be estimated
as follows:
Channels 0-10 (92 eV - 20 keV): B(E) = B(20 keV) * (20 keV/E)
Channels 11-18 (10 eV - 87 eV): B(E) = B(20 keV) * (20 keV/E) *
43.5
where B(E) is the background level (in units of cm-2 s-1 ster-1
eV-1) at energy E. The background is typically negligible at
energies below about 1 keV. Background correction is essential at
higher energies.
Data are collected through two separate apertures that cover the
same field of view but differ in their transmission by a factor of
43.5. At low energies (10 eV to 100 eV), the smaller aperture is
used to attenuate high fluxes, and at high energies (100 eV to 20
keV), the larger aperture is used to maximize the sensitivity to
low fluxes. The corrected count rates in energy channels 11-18
(100-10 eV) are multiplied by the factor 43.5 to compensate for the
smaller aperture size. Finally, we divide by the geometric factor
(0.02 cm2 ster) and the center energy (eV) to obtain the
differential flux (cm-2 s-1 ster-1 eV-1).
The data are organized into a table with a uniform time step for
all energy channels. Since the sampling interval is different for
different energy channels, data values are repeated within each
packet, as necessary, to enforce a uniform time step. The data are
sent via FTP to the Principal Investigator (Mario Acuna) at Goddard
Space Flight Center (GSFC), where they are incorporated with the
magnetometer data.
====================================================================
Data
====
The ERDR data set consists of a single time-ordered table. Each
record contains a time stamp and 19 data values, representing the
omnidirectional electron flux in 19 different energy channels
ranging from 10 eV to 20 keV.
====================================================================
Ancillary Data
==============
No additional ancillary data is required beyond that described for
the MAG.
====================================================================
Coordinate System
=================
The data are presented in omnidirectional format. The time tags
contained in the ER data set should be used to obtain the
corresponding spacecraft ephemeris information from the MAG data
set.
====================================================================
Software
========
Data reduction software for the ER is written in IDL.
====================================================================
Media/Format
============
The ER data are provided in the form of 20-column ascii tables.
Storage media are described in the MAG documentation.
|
DATA_SET_RELEASE_DATE |
2009-05-13T00:00:00.000Z
|
START_TIME |
1997-09-12T12:00:00.000Z
|
STOP_TIME |
1999-03-08T11:59:59.000Z
|
MISSION_NAME |
MARS GLOBAL SURVEYOR
|
MISSION_START_DATE |
1994-10-12T12:00:00.000Z
|
MISSION_STOP_DATE |
2007-09-30T12:00:00.000Z
|
TARGET_NAME |
MARS
|
TARGET_TYPE |
PLANET
|
INSTRUMENT_HOST_ID |
MGS
|
INSTRUMENT_NAME |
ELECTRON REFLECTOMETER
|
INSTRUMENT_ID |
ER
|
INSTRUMENT_TYPE |
PLASMA ANALYZER
|
NODE_NAME |
Planetary Plasma Interactions
|
ARCHIVE_STATUS |
ARCHIVED
|
CONFIDENCE_LEVEL_NOTE |
====================================================================
Confidence Level Overview
=========================
The ER is mounted on the spacecraft body, where measurements are
susceptible to spacecraft charging and FOV blockage. This ER
instrument design is typically used on a rapidly spinning
spacecraft (few seconds period), on which the disk-shaped FOV would
sweep out the entire sky in a time that is short compared with most
timescales of interest. However, since MGS spins slowly (100
minute period) during SPO, each data record covers only a small
region of the sky. Despite this limitation, the scalar flux
provided in the ERDR is suitable for identification of plasma
boundaries (bow shock, magnetic pile-up boundary, ionopause) and
following the evolution of the electron energy distribution, which
is useful for evaluation of the plasma environment and
interpretation of the magnetometer data. Any application of these
data that requires an unbiased average over all look directions
(4-pi ster) is NOT RECOMMENDED.
====================================================================
Review
======
The ERDR will be reviewed internally by the MGS MAG/ER team prior
to release to the planetary community. The ERDR will also be
reviewed by PDS.
====================================================================
Data Coverage and Quality
=========================
ER data are recorded throughout most of the 12-hr elliptical SPO
orbits of MGS. This orbit carries the spacecraft from the
unperturbed solar wind to well inside the ionosphere. Data quality
does not depend on the position of MGS along the orbit, although
the telemetry rate was highest near periapsis. Data quality is a
function of spacecraft rotation phase, since photoelectron
contamination depends on the illumination pattern.
====================================================================
Limitations
===========
The ER is mounted on the spacecraft instrument deck and has a
disk-shaped FOV that is orthogonal to the spacecraft XY plane and
nearly orthogonal to the spacecraft Y axis. (There is a 10-degree
rotation about the Z axis to minimize spacecraft obstructions in
the FOV.) This 360-degree FOV is divided into 16 angular sectors,
each 22.5 degrees wide. Throughout SPO, the ER was in
''fixed-sector'' mode, meaning that these 16 angular sectors
remained constant in the spacecraft reference frame, sweeping out
the entire sky every 1/2 of a spacecraft spin.
Parts of the spacecraft are within the instrument's FOV -- most
notably the stowed high gain antenna (HGA), which blocks ~70
degrees. Smaller amounts of blockage are caused by attitude control
thrusters and the -Y solar array gimbal and yoke assembly. One
effect this has on the measurements is to block ambient electrons
from the directions of the obstacles. This is most clearly seen at
high energies (> 100 eV), which are only slightly deflected by the
spacecraft floating potential. In addition, when these obstacles
are illuminated by the sun, they emit photoelectrons up to ~50 eV,
which can enter the ER aperture and elevate the counting rate at
low energies. The detailed signature of this effect depends on the
illumination pattern as the spacecraft rotates, which is a function
of the angles between Earth, Mars, and the Sun. These angles
varied during the course of SPO. Photoelectron contamination has
not been removed from the data; however, the presence of
contamination is readily identified in the low energy channels (<
50 eV) by a sharp (nearly discontinuous) increase in counting rate
which appears at regular 100-minute intervals. The contamination
disappears as abruptly as it appears.
For a duration of 4 minutes every 50 minutes, sunlight can directly
enter the ER aperture and scatter inside the instrument, creating
secondary electrons. A tiny fraction of these photons and secondary
electrons can scatter down to the anode and create a ''pulse'' of
spurious counts. This sunlight pulse appears at all energies, but
is most noticeable from 10 to 80 eV and above 1 keV. Sunlight
pulses have not been removed from the data.
The instrument's energy scale is referenced to spacecraft ground.
In sunlight, spacecraft ground floats a few volts positive relative
to the plasma in which the spacecraft is immersed. Electrons are
accelerated by the spacecraft potential before they can enter the
ER aperture, thus all energies are shifted upward by a few eV. In
addition to shifting the electron energy, the trajectories of low
energy electrons can be significantly bent by electric fields
around the spacecraft. Thus, the energy scale and imaging
characteristics are relatively poor at the lowest energies (10-30
eV), becoming much more accurate at higher energies.
|
CITATION_DESCRIPTION |
Mitchell, D.L., MGS-M-ER-3-PREMAP/OMNIDIR-FLUX-V1.0,
MGS Mars/Moons MAG/ER Pre-map ER Omnidirectional Flux V1.0,
NASA Planetary Data System, 2009.
|
ABSTRACT_TEXT |
The Electron Reflectometer Data
Record (ERDR) is a time ordered series of electron measurements from the
Mars Global Surveyor (MGS) Mission. Each record consists of a time tag
with 19 scalar data points representing measurements of the electron flux
in 19 different energy channels, ranging from 10 eV to 20 keV, with an
energy resolution of 25%. Each data point is a measure of the electron
flux (cm-2 sec-1 ster-1 eV-1) averaged over a 360 x 14 degree disk-shaped
field of view (FOV). (Parts of this FOV are masked because of spacecraft
obstructions, as described below.) During the Science Phasing Orbits
(SPO), the spacecraft was in Array Normal Spin (ANS) configuration, for
which the ER field of view sweeps out the entire sky (4-pi ster) every
50 minutes, which is much longer than the integration time per record
(2 to 48 sec, depending on energy and telemetry rate) and much longer
than most timescales of interest in Mars' plasma environment.
|
PRODUCER_FULL_NAME |
DAVID L. MITCHELL
|
SEARCH/ACCESS DATA |
Planetary Plasma Interactions Website
MGS Home Page
|
|