| M |
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Multi-angle |
![[MISR Eyes]](images/MISR_eyes.jpg) |
| I |
Imaging |
| S |
Spectro- |
| R |
Radiometer |
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Most satellite instruments look only straight down, or
toward the edge of the planet. To fully understand
Earth's climate, and to determine how it may be
changing, we need to know the amount of sunlight
that is scattered in different directions under natural
conditions. MISR is a new type of instrument
designed to address this needit will view the Earth
with cameras pointed at nine different angles. One
camera points toward nadir, and the others provide
forward and aftward view angles, at the Earth's
surface, of 26.1°, 45.6°, 60.0°, and 70.5°. As the
instrument flies overhead, each region of the Earth's
surface is successively imaged by all nine cameras in
each of four wavelengths (blue, green, red, and
near-infrared).
In addition to improving our understanding of the
fate of sunlight in the Earth's environment, MISR
data can distinguish different types of clouds, aerosol
particles, and surfaces. Specifically, MISR will
monitor the monthly, seasonal, and long-term trends in:
- the amount and type of atmospheric aerosol
particles, including those formed by natural sources
and by human activities;
- the amount, types, and heights of clouds; and
- the distribution of land surface cover, including
vegetation canopy structure.
These data will be used to investigate the influence of
aerosol, cloud, and surface properties on the Earth's
reflected radiation budget and climate. Spatial
samples are acquired every 275 m. Over a period of 7
minutes, a 360 km wide swath of Earth comes into
view at all nine angles. Special attention has been
paid to providing highly accurate absolute and
relative radiometric calibration using onboard hardware
consisting of deployable solar diffuser plates and
several types of photodiodes. To complement the
onboard calibration effort, a validation program of in
situ measurements is planned, involving field
instruments such as PARABOLA III, which automatically
scans the sky and ground at many angles, and a
multi-angle aircraft camera (AirMISR). Global
coverage by the space-based MISR will be acquired about
once every 9 days at the equator. The nominal
mission lifetime is 6 years.
MISR is being built for NASA by the Jet Propulsion
Laboratory in Pasadena, California. The Principal
Investigator is David J. Diner. For more information,
check out the MISR Web Site at
http://www-misr.jpl.nasa.gov.
| MISR Instrument Characteristics |
|
| Swath width |
360 km |
|
| Spectral bands |
446, 558, 672, 866 nm |
|
| Cross-track pixel size |
275 m off-nadir, 250 m nadir |
|
| Duty cycle | 50% (day only) |
|
| Data rate | 3.3 Mbps (avg), 9.0 Mbps (peak) |
|
| Mass | 149 kg |
|
| Power | 72 W (avg), 135 W (peak) |
![[EOS with MISR]](images/MISRscan_tn.jpg) |
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This computer-generated image shows the Terra spacecraft, with the MISR
instrument on board, orbiting the Earth. Direction of flight is toward the
lower left. The actual locations imaged by the 9 cameras, each with 4 color
bands, along the Earth's surface are illustrated here with
translucent surfaces. The background star field is also realistic
(Shigeru Suzuki and Eric De Jong, Solar System Visualization
Project, Jet Propulsion Laboratory). Click to enlarge
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This pair of red/green/blue color composite images was taken by the AirMISR
instrument on August 25, 1997, over the area surrounding Moffett Field,
California. They each cover an area approximately 10 km on a side and were
acquired from a NASA ER-2 aircraft flying at 20 kilometers altitude in an
approximately southward direction. Radiometric scaling using preflight
calibration coefficients and a simple line-by-line roll correction algorithm
have been applied. The imaged area straddles the waters of San Francisco Bay
near the inlet of Coyote Creek, mudflats, marshes, tidelands that are in part
utilized as salt evaporation ponds, and urban areas of Mountain View,
Sunnyvale, and adjacent communities that provide a grid of city streets,
buildings, and freeways. North is toward the top of these images, and the
sun is shining roughly from the south. For the bottom image, the camera was
pointing at 26.1 degrees forward of nadir, whereas the top image was taken
with the camera pointing 26.1 degrees aftward of nadir. The rivers and tidal
areas are brighter in the forward-viewing (left) image, illustrating that
these wet surfaces produce mirror-like reflections that are observable at
this viewing geometry (MISR Team, Jet Propulsion Laboratory).
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