Full text: XVIIIth Congress (Part B7)

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be discernable for modeling. With repeated coverage, 
time sequences of these signatures might permit analyses 
to link object databases with relational coverages of other 
physical parameters. 
Sensing Programs 
The future of remote sensing data collection is ensured by 
needs recognized by Heads-of State and by the fact that 
both government and commercial interests in the 
technology are driving development costs downward. In 
the next two years, NASA plans to inaugurate its Earth 
Observing System (EOS). It is designed as a fifteen-year 
series of low Earth orbiting satellites collecting 
reflectance, emission, and absorption spectra for 
atmospheric, hydrospheric and biospheric phenomena. 
Similarly, the European Space Agency (ESA) plans to 
launch the Environmental Satellite (ENVISAT) and the 
Japanese will launch their Advanced Earth Observing 
Satellite (ADEOS). All are multinational research and 
applications missions aimed at future operational systems. 
Many other nations also are contributing smaller satellites 
and sensors for more specific data collection programs. 
By 2010, there are scheduled to be more than 60 polar 
orbiting and geostationary satellites gathering Earth data. 
Sadly, there is not yet a broadly scoped program to 
integrate these data with ground-based and object data into 
holistic models of ecosystem evolution. In the authors’ 
view it is time to begin discussing and planning these 
system integrations. 
Data Integration 
System and data integration will necessarily involve 
reanalysis of the datasets themselves. Even though data 
are calibrated for detector sensitivity, sensor, drift, and 
other aberrations within a sensor’s lifetime, the entire 
collection of data from a suite of like sensors operating 
over long time frames need to be systematically calibrated 
between sensors. 
Another aspect of integration will involve substituting real 
data, where possible, for mathematically derived values in 
current models. With specific regard to global circulation 
models, the new long-term data sets from EOS and 
supplementary data sets now being developed that span the 
current century could provide critical testbeds for 
improving the accuracy of climate models. Progress in 
model development and improvement can be accelerated 
by comparisons of this kind, and through the continued 
intercomparison of the results of different models. 
Most important of all in the integration process, however, 
IS the need to develop strategies that link remotely 
acquired data about the environment to the genetic 
networks of individuals and genotypes, and to then 
program how species ought to react to changing 
environments. For example, measurements of ultraviolet 
radiation flux gain their greatest application today as a 
predictor of ozone concentrations related to the ozone 
hole. Those same measurements, and others like them, 
may be useful as stimuli for biological mutations and 
Species evolution, especially in high altitude areas. 
CONCLUSIONS 
Rapid. scientific progress is being made in genome 
509 
characterization, gene response mechanisms, learning 
processes, and the complexity of self-organizing systems. 
Remote sensor data sets, employed in raster and vector 
GIS and that integrated genome and atmospheric data as 
objects, could provide the framework for a genetic 
algorithm. As these databases began to assemble and 
integrate a sufficiently wide diversity of object and 
relational variables, rules could be developed directing 
their interactions based on field and laboratory 
observations. The complexity of hundreds of plant species 
interacting as individuals and as communities will never 
be fully understood, but perhaps society can learn enough 
about how ecosystems operate to at least emulate how they 
will react to human and natural stimuli. 
REFERENCES 
Carpenter, S.R., S.W. Chisholm, C.J. Krebs, D.W. 
Schindler, and  R.F. Wright, 1995. Ecosystem 
Experiments, Science, 269, pp. 324-327. 
Eastman, J.R. and M. Fulk. 1993. Long Sequence Time 
Series Evaluation Using Standardized Principal 
Components. Photogrammetric Engineering and Remote 
Sensing, 58(8), pp. 1307-1312. 
Kauffman, S. 1993. The Origins of Order: Self- 
Organization and Selection in Evolution. New York: 
Oxford University Press. 709pgs. 
Morain, S.A. 1993. Emerging technology for Biological 
Data Collection and Analysis. Annals, Missouri Botanical 
Gardens, 80 (2), pp.309-316. 
Morain, S.A. and A.M. Budge. 1996. Earth Observing 
Platforms and Sensors. Vol. 1 of Manual of Remote 
Sensing (R.A. Ryerson, editor-in-chief). Bethesda, MD: 
American Society for Photogrammetry and Remote 
Sensing. CD-ROM. 
NOAA/NESDIS. 1992. Global Change Database: Volume 
2, Experimental Calibrated Global Vegetation Index from 
NOAA’s Advanced Very High Resolution Radiometer, 
1985-1991. Boulder, CO:National Geophysical Data 
Center. CD-ROM. 
Stolum, H-H. 1996. River Meandering as a Self- 
Organization Process. Science, 271, pp. 1710-1713. 
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B7. Vienna 1996 
 
	        
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