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Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF)
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 100, NO. E8,
PAGES 16,895–16,906,
1995
Galileo multispectral imaging of Earth
Paul Geissler
Lunar and Planetary Laboratory, University of Arizona, Tucson
W. Reid Thompson
Laboratory for Planetary Studies, Cornell University, Ithaca, New York
Richard Greenberg
Lunar and Planetary Laboratory, University of Arizona, Tucson
Jeff Moersch
Laboratory for Planetary Studies, Cornell University, Ithaca, New York
Alfred McEwen
U. S. Geological Survey, Flagstaff, Arizona
Carl Sagan
Laboratory for Planetary Studies, Cornell University, Ithaca, New York
Abstract
Nearly 6000 multispectral images of Earth were acquired by the Galileo spacecraft during its two flybys. The Galileo images
offer a unique perspective on our home planet through the spectral capability made possible by four narrowband near-infrared
filters, intended for observations of methane in Jupiter's atmosphere, which are not incorporated in any of the currently
operating Earth orbital remote sensing systems. Spectral variations due to mineralogy, vegetative cover, and condensed water
are effectively mapped by the visible and near-infrared multispectral imagery, showing a wide variety of biological, meteorological,
and geological phenomena. Global tectonic and volcanic processes are clearly illustrated by these images, providing a useful
basis for comparative planetary geology, Differences between plant species are detected through the narrowband IR filters
on Galileo, allowing regional measurements of variation in the “red edge” of chlorophyll and the depth of the 1-μm water band,
which is diagnostic of leaf moisture content. Although evidence of life is widespread in the Galileo data set, only a single
image (at ∼2 km/pixel) shows geometrization plausibly attributable to our technical civilization. Water vapor can be uniquely
imaged in the Galileo 0.73-μm band, permitting spectral discrimination of moist and dry clouds with otherwise similar albedo.
Surface snow and ice can be readily distinguished from cloud cover by narrowband imaging within the sensitivity range of Galileo's
silicon CCD camera. Ice grain size variations can be mapped using the weak H2O absorption at 1 μm, a technique which may find important applications in the exploration of the moons of Jupiter. The Galileo
images have the potential to make unique contributions to Earth science in the areas of geological, meteorological and biological
remote sensing, due to the inclusion of previously untried narrowband IR filters. The vast scale and near global coverage
of the Galileo data set complements the higher-resolution data from Earth orbiting systems and may provide a valuable reference
point for future studies of global change.
Received 9
December
1994;
accepted 18
April
1995.
Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF)
Citation: Geissler, P., W. R. Thompson, R. Greenberg, J. Moersch, A. McEwen, and C. Sagan
(1995),
Galileo multispectral imaging of Earth,
J. Geophys. Res.,
100(E8),
16,895–16,906.
Copyright 1995 by the American Geophysical Union.
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