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18 September 2009Spatial distribution of soil water content from airborne thermal and
optical remote sensing data
Spatial and temporal information of soil water content is of essential importance for modelling of land surface processes
in hydrological studies and applications for operative systems of irrigation management. In the last decades, several
remote sensing domains have been considered in the context of soil water content monitoring, ranging from active and
passive microwave to optical and thermal spectral bands.
In the framework of an experimental campaign in Southern Italy in 2007, two innovative methodologies to retrieve soil
water content information from airborne earth observation (E.O.) data were exploited: a) analyses of the dependence of
surface temperature of vegetation with soil water content using thermal infrared radiometer (TIR), and b) estimation of
superficial soil moisture content using reflectance in the visible and near infrared regions acquired from optical sensors.
The first method (a) is applicable especially at surfaces completely covered with vegetation, whereas the second method
is preferably applicable at surfaces without or with sparse vegetation. The synergy of both methods allows the
establishment of maps of spatially distributed soil water content.
Results of the analyses are presented and discussed, in particular in view of an operative context in irrigation studies.
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Katja Richter, Mario Palladino, Francesco Vuolo, Luigi Dini, Guido D'Urso, "Spatial distribution of soil water content from airborne thermal and optical remote sensing data," Proc. SPIE 7472, Remote Sensing for Agriculture, Ecosystems, and Hydrology XI, 74720W (18 September 2009); https://doi.org/10.1117/12.829508