Mean topographic slope ( • ) and confidence interval (95%) as derived from the Shuttle Radar Topography Mission (SRTM) by land cover classes.

Mean topographic slope ( • ) and confidence interval (95%) as derived from the Shuttle Radar Topography Mission (SRTM) by land cover classes.

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Burned area algorithms from radar images are often based on temporal differences between pre- and post-fire backscatter values. However, such differences may occur long past the fire event, an effect known as temporal decorrelation. Improvements in radar-based burned areas monitoring depend on a better understanding of the temporal decorrelation ef...

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... the Shrubs class, fire severity was the most important although it was closely followed by Slope and variations in the vegetation water content between post-and pre-fire images as estimated through the dNDWI. Variable importance by land cover classes was related to the mean topographic slope (Table 2). Aspect and Slope showed high importance over Herbaceous and Shrubs classes which covered higher topographic slopes when compared to the Crops and Forests classes ( Table 2). ...
Context 2
... importance by land cover classes was related to the mean topographic slope (Table 2). Aspect and Slope showed high importance over Herbaceous and Shrubs classes which covered higher topographic slopes when compared to the Crops and Forests classes ( Table 2). The reduced importance of Aspect and Slope on the decorrelation process for the Crops class was explained by its location on low lying terrain when compared to the remaining land cover classes ( Figure 6). ...

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... After a fire event, the leaves are charred if not completely burned, thus not contributing to the volume scattering as much as healthy leaves [48,49]. As explained in [50], diverging trends in C-band post-fire backscattering can also be attributed to vegetation death changing the structure of the canopy, leaving dry branches and a minimum number of dead leaves. ...
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