3.1. Observational Requirements
3.1.1. Resolution
3.1.2. Landing Site Visibility and Field of View
3.1.3. Nesting Coverage
3.1.4. Nesting Scale Ratio
3.2. Mission Constraints
3.3. Method and Procedures/Anticipated Results
3.4. Observational Approach/ Operational Scenario
Table 1 outlines science requirements based on either science or context
arguments as noted in the preceding sections. Table 2 outlines mission
constraints as imposed by the Announcement of Opportunity and Payload
Information Package. Some of these requirements and constraints are discussed
in more detail below.
Table 1: Science Requirements for MARDI
Resolution (Highest) ~2 cm/pixel
Landing site visibility must be seen in last frame; desire to see
throughout descent
Field of View landing site visible in last frame that
covers >=10 m @ 2 cm/pixel
Nesting Coverage full for anticipated horizontal velocities
(PIP Addendum 1)
Nesting Scale Ratio better than 5:1 (<= 2:1 goal)
MTF @ Nyquist 0.10
SNR >= 20:1, for Albedo = 0.10, at aphelion,
with illumination angle (i) <= 75° (sun
elevation >= 15° )
Photometry 5% relative (within an image), 10% absolute
(between images)
Images Returned ~8-16
Spectral Response 500 to 800 nm
Bit Error Rate 5 X 10-5
A resolution goal of 2 cm/pixel was deemed necessary to adequately characterizethe local environment of the lander. It is unlikely that a surface camera will
be able to place the lander in local context as well as a camera looking down
from above the surface. Both the highly oblique viewing geometry and the
likely presence of obstacles makes reliance solely on a surface camera
subsystem for such context, risky. The 2 cm/pixel requirement is also
technically reasonable given present CCD pixel size and number, and other
requirements outlined below for viewing the actual landing site.
The requirement to view the landing site throughout the descent directly
constrains the FOV, as does the areal coverage and resolution of the last frame
(10 m at 1-2 cm/pixel). High horizontal relative to vertical velocities,
pendulum sway while descending beneath the parachute, and the desire for
oblique viewing geometry over part of the field (to provide stereoscope
coverage as well as a visual impression of relief) argue for a wide field of
view. Rapid descent and small pendulum swing argue for a narrow field of view.
Although the Mars Surveyor '98 Lander descends very rapidly (See Section 3.3.),
uncertainties in pendulum swing and horizontal wind speeds during the descent
from 8 km to 1.5 km argues for a wide field of view.
Nesting coverage is the way successive images relate to one another,
and to the entire suite of images. Full nesting means that all higher
resolution images are fully contained within the lowest resolution
image (Figure 1, right).
This provides a direct view of a small, localized area (including the
landing site) at all resolutions down to the surface, and occurs when,
for example, the descent is entirely vertical. The rapid Mars
Surveyor '98 Lander descent makes full-nesting relatively easy to
achieve.
The nesting scale or resolution ratio is determined at the beginning of descent
imaging by the altitude at which imaging starts and by the descent rate, and at
the end of the descent by the descent rate, the minimum time between frames,
and the available buffer space. An optimized solution would have a variable
nesting ratio, but practical requirements suggest that a single ratio be used
throughout the descent. For illustrative purposes, and based on the
(relatively arbitrary) data volume limit of 37 Mbits, a ten frame sequence
acquired at a ratio of roughly 2:1 (modulated primarily by the
one-every-other-second read-out speed) is illustrated in this proposal (see
Section 3.3. and Table 3, below).
In addition to the observational requirements, mission parameters also
constrain instrument design. Some of these constraints are operational (e.g.,
the location, altitude, and attitude of the spacecraft as a function of time),
while others are environmental (e.g., the thermal and ionizing radiation
environment). Additionally, there are the constraints imposed on resources,
including mass, power, and downlink data rate. Some of the values given in the
PIP and summarized in Table 2 were taken as guidelines for the various
constrained parameters.
Table 2: Mars Surveyor '98 Lander Mission Constraints for MARDI
Descent Rate/Duration 80 sec to descend 8 km, 30 sec to descend
last 1.4 km
Downrange Distance < 2 km in 80 sec, < 500 m in last 30 sec
Pendulum Angle <= 15°
Data Volume 37 Mbits (Mb) (equivalent to 1 transmission
to relay)
Computational Resources <= 2 MIPS during descent; fraction of 500 Kb
EEPROM, 1 Mb SRAM for software
Power 5 W total science during descent; 28 V
unregulated
Mass Fraction of 20 Kg total payload mass
Communications RS-422, 1 Mb/sec (2 available)
Thermal Cruise: -20° to +30° ; Operations:
-40° to +30° C
Other Physical As described in PIP
Environments (Vibration,
Shock, Acoustics,
Acceleration)
Monopropellant Engine 30° cones, 5 m in length; optically
Plume transparent; thermal distortion TBD
Radiation Total dose: ~2,500 rads at outer surface of
instrument from external sources during
cruise (assuming 0.1 inch Al shielding from
spacecraft)
MARDI acquires images every two seconds from the time the aeroshell is released
until the spacecraft lands. A fixed exposure/fixed aperture system is
employed, with the detector full-well tuned to the anticipated range in
illumination conditions. The large dynamic range is accommodated by
square-root encoding (video compress/expand = companding). Quarter-millisecond
exposures provide smearless images at all altitudes during the descent. Each
image is read off the detector in just under two seconds, with companding,
analog-to-digital conversion, video correction, and lossless data compression
occurring in realtime. The data are transmitted to the spacecraft for storage,
where a sieving algorithm selects from the acquisitions those that meet the
nesting resolution ratio criteria, retains these and releases storage for
future images (an alternative strategy uses the spacecraft's knowledge of
altitude from the altimeter to trigger image acquisitions, but use of this
strategy must await more detailed knowledge of the spacecraft). MARDI software
running on the spacecraft central processing unit (CPU) decompresses the images
and recompresses them using a lossy compressor, to reduce the volume to be
transmitted to Earth. Depending on the downlink availability and long-term
storage available, the lossless data may be retained for ultimate transmission
to Earth.
Upon receipt on Earth, the images are decompressed and pre-flight
photometric and geometric corrections are applied. Science analyses
will include extraction of relief from stereo images and production of
maps of the landing site in near-realtime in support of lander
operations. A highlight of the data processing will be the recreation
of the descent in animated form.
Table 3: Representative Descent Image Acquisition Scenario
Time Altitude Image Size Resolution Compress. Cumulative Data
(sec) (m) (m) (cm) Factor Vol. (Mb)
72 6,750 8,647 865 10:1 8.39
50 3,368 4,315 431 10:1 12.58
34 1,668 2,137 214 10:1 16.78
24 862 1,104 110 10:1 20.97
18 470 602 60.2 10:1 25.17
12 198 254 25.4 2:1 29.36
8 82 105 10.5 2:1 33.55
6 44 56 5.64 2:1 34.39
4 19 24 2.43 2:1 35.23
2 7 9 0.90 2:1 36.07
Under nominal circumstances, and limited by the available storage volume, ten
1000 X 1000 pixel images will be acquired from altitudes below 8 km. More
images could be returned if data volume were available. Table 3 provides
representative information about these images from an example operational
scenario. In general, the first image will cover about 8-9 km on a side at a
resolution of about 8-9 m/pixel, and the worst case last image (acquired 2
seconds before landing), will cover an area just under 9 m across at 0.9
cm/pixel.
In addition to the individual images, derived information will include:
- detailed geologic, geomorphic, and traverse planning maps of the landing
site, ranging in scale from 1:24K to 1:30;
- relief maps of the landing site, at scales from 1:14K to 1:80,
with vertical resolution ranging between 4 m and 2 cm; and
- time-sequential "realtime" descent animation, showing the 30 second descent
to the surface.
Descent image acquisition will be keyed to the descent ground and time
profile. Figure 4 shows the descent profile, at
two scales, as determined from information provided in the PIP and QA2
Attachment 1 (MSP Lander Terminal Descent Profile). The left hand
graph shows the profile from aeroshell deployment to touchdown in two
second increments (circles), with image acquisitions indicated by
filled circles. The total descent takes roughly 80 seconds, with the
last 30 seconds under monopropellant engine power. During the first
50 seconds, the pitch angles are relatively low (the lander is
suspended beneath the parachute) and the horizontal velocity increases
slightly owing to wind interactions in the thickening atmosphere.
Shortly after powered descent begins, the lander is pitched so that
its thrust vector is aligned with the descent velocity vector, and the
two vectors are matched throughout the terminal descent. The descent
is nearly vertical during the last 200 m.
Figure 4: Mars Surveyor '98 Descent Profile and Descent Imager Data
Acquisitions
The descent imaging sequence begins when the instrument is powered-up and the
spacecraft CPU boots the camera software around the time of parachute
deployment. Acquisition of nested images begins as soon as the aeroshell is
jettisoned, approximately 10 seconds later (altitude ~6 km). Images at that
altitude will cover just under 75 km2 at a resolution of 8.5
m/pixel. A sieving algorithm (or alternatively, altimeter-triggered
acquisitions) will be employed to acquire images at known scale intervals.
Observations at a scale ratio of 2 would yield a data set summarized in Table
3, and illustrated by the image sequence shown in Figures 1-3 (except for the
last four frames). Both lossless and lossy software compression are applied to
fit the sieving fractions and selected frames within the 37 Mb constraint;
acquisitions triggered by the altimeter could be retained in losslessly
compressed format. Following the landing, images would be compressed for
"quicklook" transmission to Earth via either direct or relay links. Owing to
its short operational life, MARDI operations will be conducted by the same
Malin Space Science Systems staff responsible for operating the Mars Global
Surveyor Relay (the MR uses the Mars Orbiter Camera solid state buffer and
error encryption processing), using software developed to support the Mars '96
landers. This will insure that the data are acquired during the first
available relay pass. Data processing will be conducted in "receipt realtime,"
and released for public dissemination and scientific analysis.