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Title: Numerical experiment on the effects of regional atmospheric pollution on global climate

Abstract

The 1973 Rand version of the Mintz-Arakawa model of the general circulation of the atmosphere was used to study the consequences of high concentrations of hygroscopic aerosols in a limited geographic region. The experiment was designed to investigate effects of the activity of the aerosol as condenstion nuclei and the consequent abnormal production of cloudiness and alteration of precipitation were of primary concern. Values of meteorological parameters generated by the experiment were compared with values simulated by a control (in which the polluted area was absent). Cloudiness increased over the polluted area and the temperature at the surface and in the lower atmosphere became warmer. Rainfall, however, was not significantly altered in the polluted region in spite of changes in the parameterization of rain that would make rainfall more difficult with a given atmospheric structure. The data suggest a possible connection between North American pollution and South American rainfall. Comparison of data from the experiment and the control indicate that in the experiment, rainfall decreases gradually and steadily within a large area of South America centered on the equator. The immediate cause is the movement of the region of maximum moisture convergence northward, toward the polluted area, while it ismore » at the same time decreasing in value. The movement is clear and the rainfall changes were found to be statistically significant. Although possible causes are discussed, the model does not properly simulate the hydrological cycle in the tropics, and a definitive explanation of decreasing rainfall in South America is marred by an unrealistic, unstable, moisture-convergence/rain cycle that occurs in the primary control. This behavior of the model precludes a conclusion that North America pollution will cause decreased tropical rainfall, but the data are sufficiently suggestive that this possibility should be examined in future investigations.« less

Authors:
Publication Date:
OSTI Identifier:
5479457
Resource Type:
Journal Article
Journal Name:
J. Appl. Meteorol.; (United States)
Additional Journal Information:
Journal Volume: 14:6
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; AIR POLLUTION; ENVIRONMENTAL EFFECTS; PARTICULATES; ECOLOGICAL CONCENTRATION; ATMOSPHERIC CIRCULATION; ATMOSPHERIC PRECIPITATIONS; CLIMATES; CLOUD COVER; CONDENSATION NUCLEI; ENVIRONMENTAL TRANSPORT; GLOBAL ASPECTS; HYDROLOGY; RAIN; MASS TRANSFER; PARTICLES; POLLUTION; 500200* - Environment, Atmospheric- Chemicals Monitoring & Transport- (-1989)

Citation Formats

Koenig, L R. Numerical experiment on the effects of regional atmospheric pollution on global climate. United States: N. p., 1975. Web. doi:10.1175/1520-0450(1975)014<1023:ANEOTE>2.0.CO;2.
Koenig, L R. Numerical experiment on the effects of regional atmospheric pollution on global climate. United States. https://doi.org/10.1175/1520-0450(1975)014<1023:ANEOTE>2.0.CO;2
Koenig, L R. 1975. "Numerical experiment on the effects of regional atmospheric pollution on global climate". United States. https://doi.org/10.1175/1520-0450(1975)014<1023:ANEOTE>2.0.CO;2.
@article{osti_5479457,
title = {Numerical experiment on the effects of regional atmospheric pollution on global climate},
author = {Koenig, L R},
abstractNote = {The 1973 Rand version of the Mintz-Arakawa model of the general circulation of the atmosphere was used to study the consequences of high concentrations of hygroscopic aerosols in a limited geographic region. The experiment was designed to investigate effects of the activity of the aerosol as condenstion nuclei and the consequent abnormal production of cloudiness and alteration of precipitation were of primary concern. Values of meteorological parameters generated by the experiment were compared with values simulated by a control (in which the polluted area was absent). Cloudiness increased over the polluted area and the temperature at the surface and in the lower atmosphere became warmer. Rainfall, however, was not significantly altered in the polluted region in spite of changes in the parameterization of rain that would make rainfall more difficult with a given atmospheric structure. The data suggest a possible connection between North American pollution and South American rainfall. Comparison of data from the experiment and the control indicate that in the experiment, rainfall decreases gradually and steadily within a large area of South America centered on the equator. The immediate cause is the movement of the region of maximum moisture convergence northward, toward the polluted area, while it is at the same time decreasing in value. The movement is clear and the rainfall changes were found to be statistically significant. Although possible causes are discussed, the model does not properly simulate the hydrological cycle in the tropics, and a definitive explanation of decreasing rainfall in South America is marred by an unrealistic, unstable, moisture-convergence/rain cycle that occurs in the primary control. This behavior of the model precludes a conclusion that North America pollution will cause decreased tropical rainfall, but the data are sufficiently suggestive that this possibility should be examined in future investigations.},
doi = {10.1175/1520-0450(1975)014<1023:ANEOTE>2.0.CO;2},
url = {https://www.osti.gov/biblio/5479457}, journal = {J. Appl. Meteorol.; (United States)},
number = ,
volume = 14:6,
place = {United States},
year = {Wed Jan 01 00:00:00 EST 1975},
month = {Wed Jan 01 00:00:00 EST 1975}
}