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ACE-2 North Atlantic Regional Aerosol Characterization Experiment

June 16 - July 25, 1997

 

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Seattle Conference Poster on Clear Column Closure Studies by Russell et al.


Clear column closure studies of urban-marine and mineral-dust aerosols using aircraft, ship, and satellite measurements in ACE-2

TITLE:Clear column closure studies of  urban-marine and mineral-dust aerosols using aircraft, ship, and satellite  measurements in ACE-2 AEROSOL CHARACTERIZATION EXPERIMENT-2 ACE-2 LOGO
ABSTRACT IMAGE OF PELICAN AIRCRAFT ACE-2 PAYLOAD SHCEMATIC DEPLOYMENT OF PLATFORMS IN ACE-2 EXPERIMENT AREA
PARTICLE RADIUS VS. CUMULATIVE OPTICAL DEPTH CONTRIBUTION CONCLUSION COMPARISONS MEASUREMENTS
MEASUREMENTS CONTINUED FIGURE 4. LEFT PANEL WAVELENGTH VS. AOD. RIGHT PANEL AEROSOL EXTINCTION VS. ALTITUDE blank page CONCLUSIONS CONTINUED
COMPARISONS CONTINUED FIG5 COMPARISON OF WATER VAPOR PROFILES AND COLUMNAR AMOUNTS DERIVED FROM AATS-14 AND DIRECT SAMPLING LEFT PANEL AOD VS. ALTITUDE RIGHT PANEL EXTINCTION VS. ALTITUDE FIG4 LEFT PANEL:CASE WITH AN AFRICAN DUST LAYER PRESENT. RIGHT PANEL: VERTICAL PROFILES OF AEROSOL EXTINCTION COEFFICIENT FOR THE LEFT PANEL CASE
CAN THE AIRBORNE SUNPHOTOMETER BE OVERESTIMATING AEROSOL LAYER OPTICAL DEPTHS? REFERENCES COMPARISONS CONTINUED FIG7. COMPARISON OF AEROSOL LAYER OPTICAL DEPTH SPECTRA DERIVED FROM AATS-14, NEPHELOMETER AND SIZE DISTRIBUTION MEASUREMENTS
FIG8. COMPARISON OF AEROSOL LAYER OPTICAL DEPTH SPECTRA FOR MARINE BOUNDARY LAYER ONLY. FIG9. COMPARISON OF AEROSOL LAYER OPTICAL DEPTH SPECTRA FOR DUST ONLY CAN THE AIRBORE SUNPHOTOMETER BE OVERESTIMATING AEROSOL LAYER OPTICAL DEPTHS CONTINUED REFERENCES CONTINUED

 

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