Quantitative estimation of tropical forest cover by SAR

The potential of spaceborne synthetic aperture radar (SAR) for monitoring tropical forest areas is assessed, using three ERS images from the Tapajos region of Amazonia gathered in 1992 and a single JERS-1 image of the same area acquired in 1993. The multitemporal ERS-1 data indicate that primary for...

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Bibliographic Details
Published in:IEEE transactions on geoscience and remote sensing 1999-01, Vol.37 (1), p.479-490
Main Authors: Grover, K., Quegan, S., da Costa Freitas, C.
Format: Article
Language:English
Subjects:
Applied geophysics
Backscatter
Displays
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Exact sciences and technology
Internal geophysics
Monitoring
Pollution, environment geology
Radar detection
Radar imaging
Satellites
Soil moisture
Spaceborne radar
Surfaces
Synthetic aperture radar
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Summary:The potential of spaceborne synthetic aperture radar (SAR) for monitoring tropical forest areas is assessed, using three ERS images from the Tapajos region of Amazonia gathered in 1992 and a single JERS-1 image of the same area acquired in 1993. The multitemporal ERS-1 data indicate that primary forest areas display a very stable radar backscattering coefficient (/spl sigma//sup 0/), while in some cases, disturbed areas (nonforest and regenerating forest) exhibit changes that appear to be associated with soil moisture variations. To counteract /spl sigma//sup 0/ distortions caused by topography, change detection based on ratios of intensity images (or differences of log images) provides a more useful discrimination approach than /spl sigma//sup 0/ variations in single images. Change detection techniques are compared, and their ability to classify primary and disturbed forest is quantitatively assessed, assuming that a land cover map inferred from a 1992 Landsat thematic mapper (TM) image is correct. Even in the best case, less than 50% of the disturbed forest region is detected in the ERS-1 images. This figure may be improved by more frequent image acquisition, but there are fundamental limitations in using C-band data since the effects of soil moisture changes on /spl sigma//sup 0/ are masked once even comparatively low levels of standing biomass are present. At the longer wavelength of JERS-1, much better discrimination is possible, but the correction of topographic distortions is likely to present problems.
ISSN:0196-2892
1558-0644
DOI:10.1109/36.739096