tration
grams
yy the
r with
ed for
use of
RR)
AC)
'eneral
nd low
itoring
e joint
tration
ise of
age of
change
ategies
pected
ied for
3. LANDSAT-7
Another long-term U.S. government satellite program which
began in 1972 is Landsat. Landsat-7, the next planned mission
after the ill-fated unsuccessful launch of Landsat-6, will be a
joint venture between NASA, NOAA and the U.S. Geological
Survey (USGS). It is also a part of NASA's Mission to Planet
Earth (MTPE) which is dedicated to monitoring the
environment and assessing global change (Asrar and
Greenstone, 1995).
Orbital parameters for Landsat-7 are designed to provide
continuity of data with those obtained by previous Landsat
satellites. The primary sensor is the Enhanced Thematic
Mapper Plus (ETM+) (Table 3). The ETM+ will acquire data
of increased spatial resolution for panchromatic (15 m) and
thermal infrared (60 m) bands. This improved resolution will
permit better characterization and monitoring of land
cover/processes. Procedures are also in place for more rapid
data dissemination to the user.
Table 3. Landsat-7
Satellite
1998 launch from 705 km Altitude
Sun Synchronous Orbit (98°)
10:00 am Descending Node Orbit
Ground Track Repeat Interval 16 Days
Sensor
Enhanced Thematic Mapper+ (ETM+)
8 Bands (1 Pan at 15 m, 6 VNIR and SWIR at 30 m,
1 TIR at 60 m)
3.8 Gb per Scene (185 x 170 km)
Solid State On-Board Storage 380 Gb or 100 Scenes
Data
USGS EROS Data Center - Process 250 Scenes per Day
Deliver up to 100 Scenes per Day to User
Data to be Available for Order within 24 hrs of
Acquisition
4. EARTH OBSERVING SYSTEM (EOS)
The Earth Observing System (EOS) is the centerpiece of
NASA’s MTPE and a key component of the U.S. Global
Change Research Program. Beginning in 1998, EOS will
consist of a series of Earth remote sensing spacecraft, each
carrying up to six instruments and launched every three to five
years (Asrar and Greenstone, 1995). In this way, continuous
data will be provided over the 15 year lifetime of the program
for observation of the atmosphere, oceans and Earth’s surface.
EOS AM-1 is scheduled for launch in mid-1998 and will
include five sensors (Table 4). Of these, the Moderate-
Resolution Imaging Spectroradiometer (MODIS) and the
Advanced Spaceborne Thermal Emission and Reflection
Radiometer (ASTER) sensors are most applicable for land
resource mapping applications.
935
Table 4. Sensors On-Board EOS AM-1
CERES - Clouds and Earth’s Radiant Energy System
MISR - Multi-angle Imaging SpectroRadiometer
MODIS - Moderate Resolution Imaging
Spectroradiometer
MOPITT - Measurements of Pollution in the
Troposphere
ASTER - Advanced Spaceborne Thermal Emission and
Reflection Radiometer
The 36 band MODIS sensor is designed to measure
biologicaland physical processes (at 250 to 500 m spatial
resolution) on a global scale every one to two days (Table 5).
Slated for both EOS AM and PM satellite series, MODIS will
provide long-term observations of global changes, Earth
surface processes and the lower atmosphere.
Table 5. EOS MODIS Sensor
Satellite
705 km Altitude
Sun Synchronous Orbit (98.2°)
10:30 am Descending Node
Ground Track Repeat Interval 16 Days
Sensor
MODIS - Moderate Resolution Imaging
Spectroradiometer
36 Bands (VNIR, SWIR, TIR at 250 m, 500 m or 1 km)
Share of Solid State On-Board Storage of 140 Gb
Revisit Time (with cross-track tilt) of 2 Days
Data
Primary Data Return via TDRSS
The Advanced Spaceborne Thermal Emission and Reflection
Radiometer (ASTER) is a joint venture between U.S. and
Japanese scientists that will provide data of high spatial
resolution (15 to 90 m) from visible to thermal infrared
wavelengths (Kahle, et al., 1991; Table 6). This information
will be used for long-term monitoring of the land surface,
water, ice and clouds (Asrar and Greenstone, 1995). A number
of mapping applications are planned for ASTER data such as
vegetation, land use patterns, hydrology, geology and surface
topography. Of primary interest to the mapping community is
the capability of generating digital elevation models (DEMs)
from the along-track stereo image data made possible by
simultaneous acquisition of nadir and aft pointing images
(Arai, 1992; Welch and Lang, 1994; Welch, 1995).
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B4. Vienna 1996