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Modelling high arctic percent vegetation cover using field digital images and high resolution satellite data
Institution:1. Geospatial Laboratory for Environmental Dynamics, Department of Natural Resources and Society, University of Idaho, 875 Perimeter Dr MS 1142, Moscow, ID 83844, USA;2. McCall Outdoor Science School, University of Idaho, McCall, ID 83638, USA;3. Lamont-Doherty Earth Observatory, Columbia University, 61 Rte 9W, Palisades, NY 10964, USA;4. Department of Earth and Environmental Sciences, Columbia University, Mail Code 5505, New York, NY 10027, USA;5. Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr. MS 233-300, Pasadena, CA 91109, USA;6. Department of Ecology, Evolution, and Environmental Biology, Columbia University, 1200 Amsterdam Avenue, New York, NY 10027, USA
Abstract:In this study, digital images collected at a study site in the Canadian High Arctic were processed and classified to examine the spatial-temporal patterns of percent vegetation cover (PVC). To obtain the PVC of different plant functional groups (i.e., forbs, graminoids/sedges and mosses), field near infrared-green-blue (NGB) digital images were classified using an object-based image analysis (OBIA) approach. The PVC analyses comparing different vegetation types confirmed: (i) the polar semi-desert exhibited the lowest PVC with a large proportion of bare soil/rock cover; (ii) the mesic tundra cover consisted of approximately 60% mosses; and (iii) the wet sedge consisted almost exclusively of graminoids and sedges. As expected, the PVC and green normalized difference vegetation index (GNDVI; (RNIR ? RGreen)/(RNIR + RGreen)), derived from field NGB digital images, increased during the summer growing season for each vegetation type: i.e., ~5% (0.01) for polar semi-desert; ~10% (0.04) for mesic tundra; and ~12% (0.03) for wet sedge respectively. PVC derived from field images was found to be strongly correlated with WorldView-2 derived normalized difference spectral indices (NDSI; (Rx ? Ry)/(Rx + Ry)), where Rx is the reflectance of the red edge (724.1 nm) or near infrared (832.9 nm and 949.3 nm) bands; Ry is the reflectance of the yellow (607.7 nm) or red (658.8 nm) bands with R2’s ranging from 0.74 to 0.81. NDSIs that incorporated the yellow band (607.7 nm) performed slightly better than the NDSIs without, indicating that this band may be more useful for investigating Arctic vegetation that often includes large proportions of senescent vegetation throughout the growing season.
Keywords:Arctic vegetation  Percent vegetation cover (PVC)  Normalized difference vegetation index (NDVI)  Camera  Object-based image analysis (OBIA)
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