P.A. Durkee, K. Ruppe and C. Skupniewicz
Department of Meteorology
Naval Postgraduate School, Monterey, CA 93943
408-656-3465
Telemail: omnet/p.durkee
This paper addresses the indirect impact of aerosols on climate through
modification of cloud microphysical structure and subsequent radiative
characteristics, as observed during the Atlantic Stratocumulus Transition
Experiment (ASTEX). During ASTEX a large variation aerosol concentration was
observed. The first half of the experiment (1-14 June 1992) was conducted in
relatively clean, marine conditions with total aerosol number concentrations of
300-700 cm-3. From 14-16 June a large plume of continental aerosols
(containing urban pollution and desert dust) moved off the Iberian Penninsula
into the operating area. The aerosol number concentrations during the
remainder of the experiment (through 27 June) were typically 2000-5000
cm-3. Satellite analysis of aerosol and cloud characteristics from
the Advanced Very High Resolution Radiometer (AVHRR) on the NOAA operational
polar orbiting satellites (NOAA 10/11/12) will be described in this paper. The
aerosol optical depth and size characteristics of the continental plume will be
shown along with the resulting cloud characteristics including droplet size and
radiative properties. Individual image analysis will be presented with airmass
trajectory results to describe the sources of aerosol features and their impact
on subsequent cloud formation. An regional analysis will also be presented that
will show the regional scale radiative imact of the aerosol particles on cloud
reflectance.