2007
DOI: 10.5589/m07-047
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Wetland characterization using polarimetric RADARSAT-2 capability

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Cited by 113 publications
(33 citation statements)
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“…As this effect seems to relate to complex factors (e.g., microwave incident angle, vegetation structure, density, and water levels), completely removing the effect is difficult when solely using the backscatter intensity. A potential solution is to use polarimetry decomposition [18,48] to distinguish the inundated vegetation, although it is not easy to obtain a substantial number of full polarimetry data, which is necessary for accurate polarimetry decomposition [18].…”
Section: Discussionmentioning
confidence: 99%
“…As this effect seems to relate to complex factors (e.g., microwave incident angle, vegetation structure, density, and water levels), completely removing the effect is difficult when solely using the backscatter intensity. A potential solution is to use polarimetry decomposition [18,48] to distinguish the inundated vegetation, although it is not easy to obtain a substantial number of full polarimetry data, which is necessary for accurate polarimetry decomposition [18].…”
Section: Discussionmentioning
confidence: 99%
“…We attribute the large increase in wetland detection to the use of a combination of high resolution multidate remote sensing ima- tease apart peatlands from seasonally drier, nonpeat accumulating wetlands or organic matter rich uplands, leading to an increase in accuracy. This agrees with SAR research conducted by others in mapping peatlands on flatter terrain (e.g., Bourgeau-Chavez et al, 2016;Grenier et al, 2007;Touzi, Deschamps, & Rother, 2007).…”
Section: Stocksmentioning
confidence: 99%
“…Radar remote sensing, including synthetic aperture radar (SAR), has great potential to provide spatially-distributed information on permafrost ecosystem dynamics with its ability to penetrate cloud and independence from solar illumination. A number of studies using the space-borne radar measurements have been conducted to extract information regarding the freeze/thaw cycle [1][2][3][4][5][6][7], taiga forests [8][9][10][11][12][13][14], wetlands [15][16][17] and geological features [18][19][20].…”
Section: Introductionmentioning
confidence: 99%
“…Kwok et al [11] demonstrated the usability of the co-and cross-polarization signature for characterizing changes in the relative scattering contributions in the radar signal between frozen and thawed conditions. Recently, several studies applied polarimetric processing techniques to characterize wetland classes in Canada [16] and to estimate the growing stock volume in Siberian forest [21,22].…”
Section: Introductionmentioning
confidence: 99%