1997
DOI: 10.1080/014311697217026
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A verification of the 'triangle' method for obtaining surface soil water content and energy fluxes from remote measurements of the Normalized Difference Vegetation Index (NDVI) and surface e

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Cited by 634 publications
(361 citation statements)
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“…The general idea of contextual models is that the variability in LST alone or in combination with the variability in vegetation properties is linked to the surface status, e.g. soil moisture availability or energy flux partitioning at the surface (Tomás et al 2014; Timmermans, Kustas, and Andreu 2015; Moran et al 1994; Jiang and Islam 2001; Gillies, Kustas, and Humes 1997; Gillies and Carlson 1995). If the image scene contains a wide range of vegetation covers and surface states that represent conditions from potential to no ET, all pixels of the image can be scaled between the cold/wet and hot/dry extremes within the scene.…”
Section: Introductionmentioning
confidence: 99%
“…The general idea of contextual models is that the variability in LST alone or in combination with the variability in vegetation properties is linked to the surface status, e.g. soil moisture availability or energy flux partitioning at the surface (Tomás et al 2014; Timmermans, Kustas, and Andreu 2015; Moran et al 1994; Jiang and Islam 2001; Gillies, Kustas, and Humes 1997; Gillies and Carlson 1995). If the image scene contains a wide range of vegetation covers and surface states that represent conditions from potential to no ET, all pixels of the image can be scaled between the cold/wet and hot/dry extremes within the scene.…”
Section: Introductionmentioning
confidence: 99%
“…The LST-SAT relationship is dependent on soil moisture (SM) for sites with low NDVIs, since wet soils exchange latent heat mainly, leaving LST similar to SAT, and dry soils give large LST-SAT differences. The relationship between LST and NDVI results in a triangular shape and the slope of the curve has been related to SM [18] and surface evapotranspiration. Unfortunately, neither SM remotely-sensed products nor ground data were available at the spatial resolution of the study.…”
Section: Geographical Datamentioning
confidence: 99%
“…Unfortunately, neither SM remotely-sensed products nor ground data were available at the spatial resolution of the study. LST and NDVI variables, which some authors use for SM estimation [18], were already included in the SAT approach. Finally, Ninyerola et al [14] considered geographical variables as important climate factors to include.…”
Section: Geographical Datamentioning
confidence: 99%
“…Both masks also remove pixels contaminated with clouds. Once the area has been separated into land and sea, the land region is analysed using the LST estimation procedure described in [5], [6], [9], while the sea area is processed using the algorithm defined in [11] for SST estimation. After both procedures are accomplished, the hybrid result (containing data from both sources) is returned in the form of a single product.…”
Section: Fig 5 Lst/vi Space Graphic Representation Containing Lst Dmentioning
confidence: 99%