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31. Beijing 2008
The International Archives of the Photogrammetry. Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part Bl. Beijing 2008
rom satellite data
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GSD [m|
□ • Mapping CD - Forestry 0 - Agriculture CD - Disaster Monitoring
0-Geology 0 - Oceanography 0- Hydrology 0 - Meteorology
Figure 2. Earth observation request: GSD versus
spectral resolution
Figure 3. Earth observation request: GSD vs revisit time
3.2 Example Disaster Monitoring: The Micro-Satellite BIRD
IO 5 -x
• Cyclones and storms,
• El Nino,
• floods,
• fires,
• volcanic activities,
• earthquakes,
• landslides,
• oil slicks,
• environmental pollution,
• industrial and power plant disaster,
we need to focus on one specific category. In this paper, the fire
categon^may serve as an example of how to approach the prob
lem of defining and developing a small satellite system in order
to improve the actual fire monitoring and fire parameter as
sessment situation.
The micro-satellite BIRD (Bi-spectral InfraRed Detection) is
used to describe a possible approach for detection and quantita
tive characterisation of high-temperature events like vegetation
fires on the Earth surface (BrieB et al., 2003). BIRD was suc
cessfully piggyback launched by an Indian Polar Satellite
Launch Vehicle (PSLV-C3) in a circular sun-synchronous orbit
with an altitude of 572 km on 22 October 2001.
Both the global change scientific community and the fire fight
ing authorities demand new and dedicated space-borne fire
observation sensors with resolution of 50-100 m for lo
cal/regional monitoring and of a few hundred metres for global
observations that would be able to detect fires from a few to a
few tens of square metres and to estimate quantitatively vari
ables such as location, temperature, area, energy release, associ
ated aerosol and gaseous emissions.
The existing satellite sensors with 3-4 pm mid-infrared channels
(AVHRR/NOAA, MODIS/TERRA, GOES) used so far to
provide data on active fires on Earth have limited spatial resolu
tion of 1 km or coarser and a low-temperature saturation of the
MIR channels (with the exception of MODIS) leading in some
cases to false alarms and preventing a quantitative characterisa
tion of larger fires.
10° J ( 1 i 1 1 1
10- 2 10- 1 10° 10' 10 2 10 3
Revisit time [days]
Figure 4. Spatial and Temporal Requirements for Coastal
Studies (after Hoepffner)
As already shown, the application areas are complex which is
indicated by the wide range of GSDs (Ground Sample Distance),
revisit times, and spectral requirements. If we concentrate on
disaster monitoring which can be further split into many catego
ries, like ,
Fine spatial resolution multi-spectral sensors like TM or ETM
on Landsat or ASTER/TERRA do not have a 3-4 pm channel,
the principal channel for daytime fire recognition. Their 2.3 pm
channels are less sensitive to smouldering fires and more af
fected by solar reflections.
The saturation limitations can be avoided using solid state
infrared detector arrays and real time digital signal processing to
provide an adaptation of the sensor radiometric dynamic range.
These are the key elements of new imaging infrared (IR) sen
sors on BIRD.
The BIRD small satellite mission is a technology demonstrator
including new infrared push-broom sensors dedicated to recog
nition and quantitative characterisation of thermal anomalies on
the Earth surface. BIRD primary mission objectives are:
• test of small satellite technologies, such as an attitude con
trol system using new star sensors and new actuators, an on
board navigation system based on a new orbit predictor and
others,test of the latest generation of infrared array sensors
with an adaptive radiometric dynamic range,
• detection and scientific investigation of High Temperature
Events (HTE) such as forest fires, volcanic activity, and
coal seam fires.