Tropospheric aerosols are thought to cause a significant direct and
indirect climate forcing, but the magnitude of this forcing remains highly
uncertain because of poor knowledge of global aerosol characteristics and
their temporal changes. The standard long-term global NOAA product, the
one-channel AVHRR aerosol optical thickness over the ocean, relies on a
single predefined aerosol model and can be inaccurate in many cases. TOMS
data can be used to detect absorbing aerosols over land, but are
insensitive to aerosols located below 1 km. It is thus clear that
innovative approaches must be employed in order to extract a more
quantitative and accurate aerosol climatology from available satellite and
other measurements, thereby enabling more reliable estimates of the direct
and indirect aerosol forcings.
This project was a response to the recommendations of the 1997 Aerosol
Workshop held at the NASA Goddard Institute for Space Studies (GISS) in
June of 1997 and the resulting call for a focused effort aimed at
extracting an improved multi-decadal aerosol record from existing satellite
measurements as outlined in the Aerosol Radiative Forcing NRA.
Specifically, the main objective has been to develop advanced global
aerosol climatologies for the full period of satellite data, supplement
them by improved modeling results, and to make these aerosol datasets
broadly available and suitable for use in studies of the direct and
indirect effects of aerosols on climate.
In the framework of GACP, multichannel aerosol retrieval algorithms, as
suggested or reviewed by the GACP Science Team, have been systematically
applied to the full period of satellite measurements. The algorithms have
been tested and refined using ground-based/in situ data and contemporaneous
EOS results. The full period of available satellite data has been
reprocessed as improved algorithms or data calibration were achieved. The
satellite retrievals over oceans and limited surface measurements have been
used to calibrate 3-D tracer aerosol models for individual aerosol types
and sources. These calibrated tracer models have thus provided an
alternative estimate of the aerosol distribution over continents. Still
further refinements of the aerosol climatologies may be possible using TOMS
and in situ/ground-based data.
The results of this project have been used in outreach programs, thus
providing a mechanism to test the use of the aerosol research as a tool for
teaching science.