We use aerosol optical depth, fire counts, and cloud fraction from Aqua-MODIS, and NCEP Reanalysis vertical velocities at 500 mb as a proxy for dynamic regime. We use daily Level-3 MODIS cloud fraction, obtained by calculating global cloud amounts from instantaneous cloud masks. We use Level-3 MODIS cloud top pressures as a measure of cloud vertical development. Since aerosols and clouds are influenced by local and regional meteorology we use daily re-gridded NCEP Reanalysis data to set the meteorological and dynamical context. Specifically, we use vertical velocities at 500 mb to account for differences in large scale dynamics and evaluate precipitable water and relative humidity as a function of aerosol to account for differences in available water vapor. In addition to MODIS we also include parallel and additional analyses with ISCCP cloud fractions (various cloud types and heights), CloudSat liquid water content, GPCP Precipitation amounts, OMI aerosol optical depth and CALIPSO aerosol types.
Preliminary results, focusing on the South American and South African biomass burning regions, indicates strong seasonal shifts the aerosol-cloud fraction relationship that varies with biomass burning activity, precipitation and region. The MRE relationship clusters with the characteristic boomerang shape during the dry season during which absorbing aerosols are present in sufficient quantities to affect cloud fraction and a distinctly different relationship during the wet season. This suggests a method for parameterizing the MRE for cloud-aerosol interactions based on seasonal shifts in precipitation and aerosol that can be incorporated into CMIP6 modeling efforts.