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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 94, NO. D6, PAGES 8381–8393, 1989

SAGE II aerosol data validation based on retrieved aerosol model size distribution from SAGE II aerosol measurements

Pi-Huan Wang

Science and Technology Corporation, Hampton, Virginia


M. P. McCormick

Atmospheric Sciences Division, NASA Langley Research Center, Hampton, Virginia


L. R. McMaster

Atmospheric Sciences Division, NASA Langley Research Center, Hampton, Virginia


W. P. Chu

Atmospheric Sciences Division, NASA Langley Research Center, Hampton, Virginia


W. H. Fuller

Atmospheric Sciences Division, NASA Langley Research Center, Hampton, Virginia


G. K. Yue

Atmospheric Sciences Division, NASA Langley Research Center, Hampton, Virginia


T. J. Swissler

ST Systems Corporation, Hampton, Virginia


M. T. Osborn

ST Systems Corporation, Hampton, Virginia


P. B. Russell

NASA Ames Research Center, Moffett Field, California


V. R. Oberbeck

NASA Ames Research Center, Moffett Field, California


J. Livingston

SRI International, Menlo Park, California


J. M. Rosen

Department of Physics and Astronomy, University of Wyoming, Laramie


D. J. Hofmann

Department of Physics and Astronomy, University of Wyoming, Laramie


G. W. Grams

School of Geophysical Sciences, Georgia Institute of Technology, Atlanta


Abstract

This paper describes an investigation of the comprehensive aerosol correlative measurement experiments conducted between November 1984 and July 1986 for the satellite measurement program of the Stratospheric Aerosol and Gas Experiment (SAGE II). The correlative sensors involved in the experiments consist of the NASA Ames Research Center impactor/laser probe, the University of Wyoming dustsonde, and the NASA Langley Research Center airborne 14-inch (36 cm) lidar system. The approach of the analysis is to compare the primary aerosol quantities measured by the ground-based instruments with the calculated ones based on the aerosol size distributions retrieved from the SAGE II aerosol extinction measurements. The analysis shows that the aerosol size distributions derived from the SAGE II observations agree qualitatively with the in situ measurements made by the impactor/laser probe. The SAGE II-derived vertical distributions of the ratio N0.15/N0.25 (where Nr is the cumulative aerosol concentration for particle radii greater than r, in micrometers) and the aerosol backscatter profiles at 0.532- and 0.6943-μm lidar wavelengths are shown to agree with the dustsonde and the 14-inch (36 cm) lidar observations, with the differences being within the respective uncertainties of the SAGE II and the other instruments. © American Geophysical Union 1989

Index Terms: 0305 Atmospheric Composition and Structure: Aerosols and particles; 0340 Atmospheric Composition and Structure: Middle atmosphere—composition and chemistry; 0394 Atmospheric Composition and Structure: Instruments and techniques; 6969 Radio Science: Remote sensing.


Citation: Wang, P.-H., et al. (1989), SAGE II aerosol data validation based on retrieved aerosol model size distribution from SAGE II aerosol measurements, J. Geophys. Res., 94(D6), 8381–8393.