HR: 1340h
AN: B33E-1076 [Abstracts]
TI: Use of JERS Satellite Imagery Mosaics for Boreal Wetlands Mapping
AU: Whitcomb, J B
EM: jane.whitcomb@sbcglobal.edu
AF: University of Michigan, 3238 EECS
1301 Beal Ave, Ann Arbor, MI 48105
United States
AU: * Moghaddam, M
EM: mmoghadd@umich.edu
AF: University of Michigan, 3238 EECS
1301 Beal Ave, Ann Arbor, MI 48105
United States
AU: Kellndorfer, J
EM: josefk@whrc.org
AF: Woods Hole Research Center, PO Box 296, Woods Hole, MA 02543
United States
AU: McDonald, K
EM: kyle.mcdonald@jpl.nasa.gov
AF: Jet Propulsion Laboratory, Mail Stop 300-233
California Institute of Technology
4800 Oak Grove Drive, Pasadena, CA 91109-8099
United States
AU: Podest, E
EM: erika.podest@jpl.nasa.gov
AF: Jet Propulsion Laboratory, Mail Stop 300-233
California Institute of Technology
4800 Oak Grove Drive, Pasadena, CA 91109-8099
United States
AB:
Wetlands play a critical role, not only in the health of boreal ecosystems, but also as significant carbon sinks and sources
whose quantification may be key in balancing the global carbon budget. An accurate assessment of the spatial and temporal
distribution of wetlands could thus be used to significantly improve estimates of the global net carbon exchange. The
locations, types, and extents of wetlands are still uncertain, however, partly because it is difficult to identify and
classify wetlands on a global scale using widely available optical remote sensing data. Low-frequency synthetic aperture
radar (SAR) is well suited to the task of identifying and classifying wetlands. Its ability to penetrate the forest canopy
has been used to advantage in characterizing vegetation structure, biomass, and moisture content. It is especially sensitive
to scattering from flooded forest swamplands, due to its ability to penetrate vegetation and reflect back from standing water
under vegetation. We have used multi-temporal L-band JERS-1 SAR imagery in order to produce a thematic map of wetlands in
the North American boreal zone. The map will identify four land cover classes based on their distinct scattering
characteristics: Open water, Herbacious wetlands (e.g., marshes, fens, bogs), Woody wetlands (e.g., swamps), and
Non-wetlands. Tasks involved in generating the map included the following: 1) training sites for each class within each
ecoregion are identified, 2) two seasons of JERS imagery are geographically co-registered with a digital elevation model
(DEM), a slope model, and an open water mask, 3) the slope model is used to mask out areas that cannot be wetlands and the
open water mask is applied to distinguish herbacious wetlands from open water, 4) the spectral characteristics of each
wetlands class as a function of imagery acquisition date and boreal ecoregion are identified, and 5) classification is
performed by a combination of the spectral/eco-regional knowledgebase with a minimum distance classifier. The performance of
the algorithm is validated using ground truth reference data from multiple wetland validation sites of known characteristics.
DE: 0497 Wetlands (1890)
SC: Biogeosciences [B]
MN: Fall Meeting 2005