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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.
Copyright 1989 by the American Geophysical Union.
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