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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 109,
D19S15,
doi:10.1029/2003JD004467,
2004
Spectral absorption of solar radiation by aerosols during ACE-Asia
R. W. Bergstrom
Bay Area Environmental Research Institute, Sonoma, California, USA
P. Pilewskie
NASA Ames Research Center, Moffett Field, California, USA
J. Pommier
Bay Area Environmental Research Institute, Sonoma, California, USA
M. Rabbette
Bay Area Environmental Research Institute, Sonoma, California, USA
P. B. Russell
NASA Ames Research Center, Moffett Field, California, USA
B. Schmid
Bay Area Environmental Research Institute, Sonoma, California, USA
J. Redemann
Bay Area Environmental Research Institute, Sonoma, California, USA
A. Higurashi
National Institute of Environmental Studies, Tsukuba, Japan
T. Nakajima
Center for Climate Systems Research, University of Tokyo, Tokyo, Japan
P. K. Quinn
NOAA Pacific Marine Environmental Laboratory, Seattle, Washington, USA
Abstract
As part of the Asian Pacific Regional Aerosol Characterization Experiment (ACE-Asia), the upward and downward spectral solar
radiant fluxes were measured with the Spectral Solar Flux Radiometer (SSFR), and the aerosol optical depth was measured with
the Ames Airborne Tracking Sunphotometer (AATS-14) aboard the Center for Interdisciplinary Remotely-Piloted Aircraft Studies
(CIRPAS) Twin Otter aircraft. In this paper, we examine the data obtained for two cases: a moderately thick aerosol layer,
12 April, and a relatively thin aerosol case, 16 April 2001. On both days, the Twin Otter flew vertical profiles in the Korean
Strait southeast of Gosan Island. For both days we determine the aerosol spectral absorption of the layer and estimate the
spectral aerosol absorption optical depth and single-scattering albedo. The results for 12 April show that the single-scattering
albedo increases with wavelength from 0.8 at 400 nm to 0.95 at 900 nm and remains essentially constant from 950 to 1700 nm.
On 16 April the amount of aerosol absorption was very low; however, the aerosol single-scattering albedo appears to decrease
slightly with wavelength in the visible region. We interpret these results in light of the two absorbing aerosol species observed
during the ACE-Asia study: mineral dust and black carbon. The results for 12 April are indicative of a mineral dust-black
carbon mixture. The 16 April results are possibly caused by black carbon mixed with nonabsorbing pollution aerosols. For the
12 April case we attempt to estimate the relative contributions of the black carbon particles and the mineral dust particles.
We compare our results with other estimates of the aerosol properties from a Sea-Viewing Wide Field-of View Sensor (SeaWiFS)
satellite analysis and aerosol measurements made aboard the Twin Otter, aboard the National Oceanic and Atmospheric Administration
Ronald H. Brown ship, and at ground sites in Gosan and Japan. The results indicate a relatively complicated aerosol mixture of both industrial
pollution (including black carbon) and mineral dust. This underscores the need for careful measurements and analysis to separate
out the absorption effects of mineral dust and black carbon in the east Asia region.
Received 18
December
2003;
accepted 3
May
2004;
published 8
September
2004.
Keywords: light absorption;
single-scattering albedo;
ACE-Asia aerosols.
Index Terms: 0305 Atmospheric Composition and Structure: Aerosols and particles (0345, 4801); 0345 Atmospheric Composition and Structure: Pollution—urban and regional (0305); 0360 Atmospheric Composition and Structure: Transmission and scattering of radiation; 3359 Meteorology and Atmospheric Dynamics: Radiative processes; 9320 Information Related to Geographic Region: Asia.
Read Full Article (file size: 1274981 bytes) Cited by
Citation: Bergstrom, R. W., P. Pilewskie, J. Pommier, M. Rabbette, P. B. Russell, B. Schmid, J. Redemann, A. Higurashi, T. Nakajima, and P. K. Quinn
(2004),
Spectral absorption of solar radiation by aerosols during ACE-Asia,
J. Geophys. Res.,
109,
D19S15,
doi:10.1029/2003JD004467.
Copyright 2004 by the American Geophysical Union.
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