Satellite retrieved aerosol optical properties are compared to aircraft mea
surements for a case study during the Tropospheric Aerosol Radiative Forcin
g Observational Experiment (TARFOX). Two satellite instruments are used: th
e Along Track Scanning Radiometer 2 (ATSR-2) and the advanced very high res
olution radiometer (AVHRR). The aerosol optical depth in the mid-visible (0
.555 mu m) retrieved from the ATSR-2 data agrees within 0.03 with colocated
sunphotometer measurements. Also, the spectral behavior of the aerosol opt
ical depth is retrieved accurately. Good correlation is found between aeros
ol optical depths for AVHRR channel 1 (0.64 mu m) and sunphotometer derived
values, but the satellite retrieved values are 0.05 to 0.15 lower. The Ang
strom wavelength exponent is determined both from the ATSR-2 and the AVHRR
data. The ATSR-2 derived Angstrom exponents are in good agreement with the
values computed from the sunphotometer data. The Angstrom exponents determi
ned from AVHRR data show very large variations. Both the ATSR-2 and the AVH
RR aerosol optical depth images show a large gradient. Vertical profile dat
a of temperature, relative humidity, and particle scattering indicate that
this gradient is probably caused by changes in the dry aerosol properties,
rather than a change in the relative humidity.