AIRCRAFT MEASUREMENTS   
             
          Intensive
          aircraft field measurements over the two sides of the bunny fence will
          be conducted during the NCAR GLASS radiosonde measurement period at
          no cost to the project.  This experiment
              will be similar to the buFex  (Bunny Fence Experiments) intensive
              field campaigns which were conducted in the 1990’s (e.g.,
              Lyons et al, 1993). 
               
              The aircraft will be instrumented with sensors capable of measuring
              all of the components of surface energy budget (Hacker and Schwerdtfeder,
              1988).  These measurements will be supplemented with simultaneous
              continuous surface observations of turbulent fluxes as well as
              standard meteorological parameters and infrared thermometry.  Results
              from previous expeditions are archived at the Western  Australian
              Remote Sensing Application Centre.  Relationships derived
              from the aircraft transects and field measurements then are used
              to characterize the large-scale variation in surface temperature,
              albedo and surface roughness and their variability throughout the
              day.  This will be accomplished by repeated overpasses across
              the bunny fence in transects between the two Bowen Ratio sites
              and on long traverses on either side of the fence.  These
              data in turn will be combined with local meteorological data to
              estimate the latent and sensible heat fluxes between native and
              agricultural vegetation.   
            As reported by
            Ray et al (2003), aircraft measurements for the time period of 1000-1100
            LST were compared to satellite-derived values taken at approximately
            1030 LST.  In general, comparisons of
            latent heat values for the satellite and aircraft measurements were
            found to be in good agreement, but with discrepancies in sensible
            heat fluxes.  The combination of simultaneous aircraft, satellite,
            radiosonde, and Bowen Ratio station observations will allow us to
            compare the various approaches and to validate them with surface
            measurements. |