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AGU: Journal of Geophysical Research, Atmospheres

 

Index Terms

  • Atmospheric Composition and Structure: Aerosols and particles
  • Atmospheric Composition and Structure: Middle atmosphere—energy deposition
  • Atmospheric Composition and Structure: Pollution—urban and regional
  • Atmospheric Composition and Structure: Transmission and scattering of radiation
  • Atmospheric Composition and Structure: Instruments and techniques
Abstract
Cited By (35)
 

Abstract

Solar spectral radiative forcing during the Southern African Regional Science Initiative

P. Pilewskie

Earth Science Division, NASA Ames Research Center, Moffett Field, California, USA

J. Pommier

Bay Area Environmental Research Institute, Sonoma, California, USA

R. Bergstrom

Bay Area Environmental Research Institute, Sonoma, California, USA

W. Gore

Earth Science Division, NASA Ames Research Center, Moffett Field, California, USA

S. Howard

Bay Area Environmental Research Institute, Sonoma, California, USA

M. Rabbette

Bay Area Environmental Research Institute, Sonoma, California, USA

B. Schmid

Bay Area Environmental Research Institute, Sonoma, California, USA

P. V. Hobbs

Department of Atmospheric Sciences, University of Washington, Seattle, Washington, USA

S. C. Tsay

NASA Goddard Space Flight Center, Greenbelt, Maryland, USA

During the dry season component of the Southern African Regional Science Initiative (SAFARI) in late winter 2000, the net solar spectral irradiance was measured at flight levels throughout biomass burning haze layers. From these measurements, the flux divergence, fractional absorption, instantaneous heating rate, and absorption efficiency were derived. Two cases are examined: on 24 August 2000 off the coast of Mozambique in the vicinity of Inhaca Island and on 6 September 2000 in a very thick continental haze layer over Mongu, Zambia. The measured absolute absorption was substantially higher for the case over Mongu where the measured midvisible optical depth exceeded unity. Instantaneous heating from aerosol absorption was 4 K d−1 over Mongu, Zambia and 1.5 K d−1 near Inhaca Island, Mozambique. However, the spectral absorption efficiency was nearly identical for both cases. Although the observations over Inhaca Island preceded the “river of smoke” from the southern African continent by nearly 2 weeks, the evidence here suggests a continental influence in the lower tropospheric aerosol far from source regions of burning.

Published 13 March 2003.

Citation: Pilewskie, P., J. Pommier, R. Bergstrom, W. Gore, S. Howard, M. Rabbette, B. Schmid, P. V. Hobbs, and S. C. Tsay (2003), Solar spectral radiative forcing during the Southern African Regional Science Initiative, J. Geophys. Res., 108(D13), 8486, doi:10.1029/2002JD002411.

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