2010
DOI: 10.3390/rs1020333
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Estimating Daily Land Surface Temperatures in Mountainous Environments by Reconstructed MODIS LST Data

Abstract: Continuous monitoring of extreme environments, such as the European Alps, is hampered by the sparse and/or irregular distribution of meteorological stations, the difficulties in performing ground surveys and the complexity of interpolating existing station data. Remotely sensed Land Surface Temperature (LST) is therefore of major interest for a variety of environmental and ecological applications. But while MODIS LST data from the Terra and Aqua satellites are aimed at closing the gap between data demand and a… Show more

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Cited by 316 publications
(213 citation statements)
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References 30 publications
(17 reference statements)
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“…DLST and NLST were used as proxies for both soil and air temperature, which play an important role in shaping tsetse habitat. Low-quality pixels were removed from the raw data using the quality assessment layer and outliers were filtered using a variant of the boxplot algorithm (37). Vegetation indices at 1 km of spatial resolution and with temporal resolution of 16 d (MOD13A2/ MYD13A2) were also downloaded and processed using the quality assessment layer.…”
Section: Methodsmentioning
confidence: 99%
“…DLST and NLST were used as proxies for both soil and air temperature, which play an important role in shaping tsetse habitat. Low-quality pixels were removed from the raw data using the quality assessment layer and outliers were filtered using a variant of the boxplot algorithm (37). Vegetation indices at 1 km of spatial resolution and with temporal resolution of 16 d (MOD13A2/ MYD13A2) were also downloaded and processed using the quality assessment layer.…”
Section: Methodsmentioning
confidence: 99%
“…Surface interpolation approaches using only temperature and no auxiliary data fail to produce realistic results in areas with complex topography [13] when the data points used for interpolation are unevenly distributed, leaving large gaps. Therefore, spatial interpolation methods should not only use the existing LST values, but also auxiliary data as predictors for LST in a statistical model.…”
Section: Reconstruction Of Remotely Sensed Temperature Mapsmentioning
confidence: 99%
“…Even though HANTS was originally developed for NDVI reconstruction, it can, in theory, also be applied to LST or any other time series showing periodicity. Regarding spatial interpolation, previously applied methods to filter and reconstruct MODIS LST values include 2D [19] and 3D [13] spline interpolation. While being a full reconstruction of all layers, the approach of Neteler et al [13] was only developed for a small region with very complex topography.…”
Section: Previous Approachesmentioning
confidence: 99%
“…Then, LSTs flagged with "average emissivity error ≤0.04 (or >0.04)" or "average LST error >3 K" were eliminated. Finally, abnormally low LSTs, determined by histogram-based quartile statistics [53], were probably caused by undetected clouds and thus filtered out. In this study, Terra nighttime LST, instead of Aqua and/or daytime LST, was chosen because it is more stable and accurate [54,55] and has a weaker angular effect [56] and a larger number of valid pixels [57].…”
Section: Spatio-temporal Predictorsmentioning
confidence: 99%