2024-03-28T14:55:05Zhttp://digital.csic.es/dspace-oai/requestoai:digital.csic.es:10261/98112018-08-03T10:14:37Zcom_10261_74com_10261_6col_10261_327
Sepulcre-Cantó, G.
Zarco-Tejada, Pablo J.
Jiménez-Muñoz, J. C.
Sobrino, J. A.
Miguel, E. de
Villalobos, Francisco J.
2009-01-22T12:36:21Z
2009-01-22T12:36:21Z
2006
Agricultural and Forest Meteorology, 136, 31-44.
0168-1923
http://hdl.handle.net/10261/9811
10.1016/j.agrformet.2006.01.008
An investigation of the detection of water stress in non-homogeneous crop canopies such as orchards using high-spatial
resolution remote sensing thermal imagery is presented. An airborne campaign was conducted with the Airborne Hyperspectral
Scanner (AHS) acquiring imagery in 38 spectral bands in the 0.43–12.5 mm spectral range at 2.5 m spatial resolution. The AHS
sensor was flown at 7:30, 9:30 and 12:30 GMT in 25 July 2004 over an olive orchard with three different water-deficit irrigation
treatments to study the spatial and diurnal variability of temperature as a function of water stress. A total of 10 AHS bands located
within the thermal-infrared region were assessed for the retrieval of the land surface temperature using the split-window algorithm,
separating pure crowns from shadows and sunlit soil pixels using the reflectance bands. Ground truth validation was conducted with
infrared thermal sensors placed on top of the trees for continuous thermal data acquisition. Crown temperature (Tc), crown minus air
temperature (Tc Ta), and relative temperature difference to well-irrigated trees (Tc TR, where TR is the mean temperature of the
well-irrigated trees) were calculated from the ground sensors and from the AHS imagery at the crown spatial resolution. Correlation
coefficients for Tc TR between ground IRT sensors and airborne image-based AHS estimations were R2 = 0.50 (7:30 GMT),
R2 = 0.45 (9:30 GMT) and R2 = 0.57 (12:30 GMT). Relationships between leaf water potential and crown Tc Ta measured with
the airborne sensor obtained determination coefficients of R2 = 0.62 (7:30 GMT), R2 = 0.35 (9:30 GMT) and R2 = 0.25
(12:30 GMT). Images of Tc Ta and Tc TR for the entire field were obtained at the three times during the day of the overflight,
showing the spatial and temporal distribution of the thermal variability as a function of the water deficit irrigation schemes.
eng
closedAccess
Thermal remote sensing
Crown temperature
Water stress
Deficit irrigation
Split-window
Detection of Water Stress in an Olive Orchard with Thermal Remote Sensing Imagery
artículo