Results of a Comprehensive Atmospheric Aerosol-Radiation Experiment in the Southwestern United States. Part II: Radiation Flux Measurements and Theoretical InterpretationSource: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 005::page 455Author:DeLuisi, J. J.
,
Furukawa, P. M.
,
Gillette, D. A.
,
Schuster, B. G.
,
Charlson, R. J.
,
Porch, W. M.
,
Fegley, R. W.
,
Herman, B. M.
,
Rabinoff, R. A.
,
Twitty, J. T.
,
Weinman, J. A.
DOI: 10.1175/1520-0450(1976)015<0455:ROACAA>2.0.CO;2Publisher: American Meteorological Society
Abstract: The experimental results in Part I are used in the theoretical interpretation of the radiation flux measurements which were taken with an aircraft. The absorption term of the complex refractive index of aerosols is estimated to be approximately 0.01 for a real part of 1.5 for the wavelength bandwidth 0.32?0.68 ?m. A regional variation in the refractive index is noted. Atmospheric heating and cooling rates due to aerosol and molecular absorption in the solar and terrestrial wavelengths are determined from the radiation flux measurements. The magnitudes of these rates are compared and their relative importance is discussed.
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contributor author | DeLuisi, J. J. | |
contributor author | Furukawa, P. M. | |
contributor author | Gillette, D. A. | |
contributor author | Schuster, B. G. | |
contributor author | Charlson, R. J. | |
contributor author | Porch, W. M. | |
contributor author | Fegley, R. W. | |
contributor author | Herman, B. M. | |
contributor author | Rabinoff, R. A. | |
contributor author | Twitty, J. T. | |
contributor author | Weinman, J. A. | |
date accessioned | 2017-06-09T17:38:35Z | |
date available | 2017-06-09T17:38:35Z | |
date copyright | 1976/05/01 | |
date issued | 1976 | |
identifier issn | 0021-8952 | |
identifier other | ams-9069.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4232516 | |
description abstract | The experimental results in Part I are used in the theoretical interpretation of the radiation flux measurements which were taken with an aircraft. The absorption term of the complex refractive index of aerosols is estimated to be approximately 0.01 for a real part of 1.5 for the wavelength bandwidth 0.32?0.68 ?m. A regional variation in the refractive index is noted. Atmospheric heating and cooling rates due to aerosol and molecular absorption in the solar and terrestrial wavelengths are determined from the radiation flux measurements. The magnitudes of these rates are compared and their relative importance is discussed. | |
publisher | American Meteorological Society | |
title | Results of a Comprehensive Atmospheric Aerosol-Radiation Experiment in the Southwestern United States. Part II: Radiation Flux Measurements and Theoretical Interpretation | |
type | Journal Paper | |
journal volume | 15 | |
journal issue | 5 | |
journal title | Journal of Applied Meteorology | |
identifier doi | 10.1175/1520-0450(1976)015<0455:ROACAA>2.0.CO;2 | |
journal fristpage | 455 | |
journal lastpage | 463 | |
tree | Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 005 | |
contenttype | Fulltext |