Text Size
NASA's DC-8 airborne science laboratory flew low over San Joaquin Valley farm fields while specialized instruments collected data during the vegetation canopy and soil moisture study. (Jane Peterson/NSERC) › View Larger Image
Morning, left, and afternoon, right, MASTER imagery of the study site consisting of three pistachio and eight almond blocks. Lightness in color on the right image indicates the lower vegetation canopy water content. Labels on left image are orchard block numbers. (University of California, Davis) › View Larger Image
Scientists seeking insight into the role vegetation plays in water fluctuation between soil and the atmosphere recently conducted research using specialized sensors during a series of NASA Airborne Science flights over California's San Joaquin Valley.
The MODIS/ASTER airborne simulator, or MASTER, instrument, shown here in a calibration lab at NASA's Jet Propulsion Laboratory, was carried on NASA's DC-8 and ER-2 aircraft to collect remote sensing data that measured evapotranspiration from almond orchards in California's San Joaquin Valley. (NASA / JPL) › View Larger Image
The G-III carries the Unmanned Aerial Vehicle Synthetic Aperture Radar designed and operated by NASA's Jet Propulsion Laboratory in Pasadena, Calif. Located in a specialized pod attached to the belly of the aircraft, the sensor acquires repeat-path data from an altitude of 41,000 feet. During four flights over the target area at solar noon, or roughly 1 p.m., in June 2010 and May, June and November 2011, the UAVSAR collected data to determine soil moisture changes. Two of the G-III's missions took place on days the ER-2 flew.
The NASA-developed Airborne Visible/Infrared Imaging Spectrometer, or AVIRIS, shown here undergoing pre-flight checkout, was carried aboard NASA's high-flying ER-2 to monitor the diurnal evapotranspiration and vegetation canopy water content changes. (NASA Ames) › View Larger Image
Along with ground-based sampling of evapotranspiration, soil moisture and vegetation water content measurements, the MASTER, AVIRIS and UAVSAR data collection at different altitudes allowed for a tracking of water changes between the ground, canopy and atmosphere throughout the day. The various hours of collection were important to this study because canopy water content has been proven to decrease from morning to afternoon.