Measurements of the Climate-forcing Properties of Atmospheric Aerosols
Aerosol Effects on Climate
Estimates of Global Mean Radiative Forcing
Placeholder (4 slides)
CAVEAT
Uncertainties Of Parameters Used To Estimate Direct Aerosol Forcing Of Climate
Scientific Questions
Sampling Strategy for CMDL Aerosol Monitoring Program
Key Aerosol Types For Evaluating Climate Forcing By Anthropogenic Aerosols
CMDL Aerosol Network
Parameters controlling aerosol forcing
Linking up-scatter optical depth to aerosol chemical composition
Aerosol climate-forcing properties observed by CMDL
KEY FEATURES OF CMDL AEROSOL SAMPLING SYSTEM
NOAA Aerosol Sampling Inlet
NOAA Aerosol Sampling System
NOAA Aerosol Sampling Rack
Arctic Haze has Decreased at Barrow, Alaska since the mid-1980’s
Aerosol single-scattering albedo at Bondville, Illinois
PPT Slide
Sensitivity of aerosol forcing to observed variation in aerosol properties at Bondville
3-D Isentropic Airmass Trajectories
Wavelength-dependence of aerosol scattering is controlled by coarse/fine mix
Aerosol Extensive Properties at Sable Island by Trajectory Sector
Aerosol Intensive Properties at Sable Island by Trajectory Sector
Hygroscopic growth at Sable Island
Aerosol Forcing Efficiency (W m-2) at Sable Island by Trajectory Sector
Calculation of aerosol optical depth from surface observations
Surface aerosol properties in southeast USA may represent the column
NOAA/CMDL Measurements of Single-scattering Albedo
Aerosol Radiative Properties in Mexico City
CMDL Aerosol Monitoring Highlights
Conclusions
Email: jogren@cmdl.noaa.gov
Home Page: /aerosol/
