618-14 Radiometric Surface Temperature Components for Row Crops.

See more from this Division: A03 Agroclimatology & Agronomic Modeling
See more from this Session: Symposium --Integrating Instrumentation, Modeling, and Remote Sensing in Honor of John Norman

Tuesday, 7 October 2008: 2:45 PM
George R. Brown Convention Center, 362DE

Paul Colaizzi1, William Kustas2, Susan O'Shaughnessy3, Robert Schwartz2, Steven Evett3, Terry Howell4, José L. Chávez4, Prasanna Gowda4 and Judy Tolk3, (1)USDA-ARS, Conservation and Production Res. Lab., Bushland, TX
(2)USDA-ARS, Beltsville, MD
(3)USDA-ARS, Bushland, TX
(4)Conservation and Production Research Laboratory, USDA-ARS, Bushland, TX
Abstract:
Land surface temperature is a boundary condition often used in assessing soil moisture status and energy exchange from the soil-vegetation-atmosphere interface. For row crops having incomplete canopy cover, the radiometric surface temperature is a composite of sunlit and shaded vegetation and substrate. Relative contributions of each temperature component are dependent on sun-target-sensor geometry. We developed a model that partitions the composite radiometric surface temperature into its respective temperature components for arbitrary orientations of the sun, row crop, and infrared thermometer viewing angle. The model assumes an elliptical sensor field-of-view overlaid on a continuous elliptical canopy. The model was tested using field measurements of vegetation, sunlit soil, shaded soil, and the soil-vegetation composite of row crops. For clear-sky conditions, dry soil, and a non-water-stressed cotton canopy, shaded soil was up to 10°C greater than vegetation; however, sunlit soil was up to 40°C greater than vegetation.

See more from this Division: A03 Agroclimatology & Agronomic Modeling
See more from this Session: Symposium --Integrating Instrumentation, Modeling, and Remote Sensing in Honor of John Norman