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Climatic Change: Volcanoes, Man-Made Pollution, and Carbon Dioxide

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TLDR
In this paper, the causes of climate change are summarized with emphasis on what appear to be the three most important factors external to atmospheric processes controlling climate on the scale of decades, i.e., high level stratospheric particles injected by volcanic eruptions, the increase in carbon dioxide due to an increase in industrial activity, and the generation of lower atmospheric particles directly caused by man.
Abstract
The causes of climatic change are summarized with emphasis on what appear to be the three most important factors external to atmospheric processes controlling climate on the scale of decades. These are 1) high level stratospheric particles injected by volcanic eruptions, 2) the increase in carbon dioxide due to an increase in industrial activity, and 3) generation of lower atmospheric particles directly caused by man. A historical perspective on each of these begins with the earliest discoveries and ends with current state of the art knowledge. The impact of these factors on climate is examined using the model of Bryson and Dittberner [30]. Results show that these three factors can indeed simulate, remarkably well, the past behavior of hemispheric climate as best we know it. The most important implication to emerge from this study is that climate is affected not only by nature, but also by man through the burning of fossil fuels and the subsequent production of carbon dioxide and particulates.

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Volcanic pollution and climate: The 1783 Laki eruption

TL;DR: The atmospheric impact of volcanic eruptions on the earth's climate is not simply related to the volume of erupted material, but relfects the chemistry of the magma, specifically the concentration of the volatile constituents SO/sub 2/, H/sub 1/S, and to a lesser extent Cl and F as discussed by the authors.
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Carbon dioxide in the urban atmosphere: Dependencies and trends

TL;DR: In this article, the authors analyzed carbon dioxide data from three urban sites in New Jersey covering periods of up to 9 years and found that the diurnal patterns appear to be influenced strongly by local mixing and turbulence conditions and seldom show the 'rush hour' peaks often found in urban carbon monoxide data.
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Carbon dioxide and climate

TL;DR: In the years 1975-1978 concern over the increase of CO2 in the atmosphere expanded from the laboratory into the public policy arena as discussed by the authors, during which a profusion of international symposia, technical papers and public-policy-oriented discussions drew wide attention to the potential dangers of unchecked growth of atmospheric CO2 and man's alterations of the global carbon cycle.
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The effects of aerosols on the response of a two-dimensional zonally-averaged climate model

TL;DR: In this article, the response of climate processes to changes in aerosols is investigated using a two-dimensional zonally-averaged climate model, where a strongly scattering maritime aerosol and a strongly absorbing rural aerosol over land are used in the layer between the surface and the 700 mb level.
References
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Journal ArticleDOI

The Maunder Minimum

TL;DR: In the years around a sunspot maximum there is seldom a day when a number of spots cannot be seen, and often hundreds are present.
Book

On the Influence of Carbonic Acid in the Air upon the Temperature of the Ground

TL;DR: The influence of carbonic acid in the air upon the temperature of the ground was examined in this article, where the influence of CO 2 on the ground temperature was investigated. But the authors focused on the effect of carbon dioxide on the air and not the ground.
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Thermal Equilibrium of the Atmosphere with a Given Distribution of Relative Humidity

TL;DR: In this article, the authors show that the surface equilibrium temperature of the atmosphere with a given distribution of relative humidity is almost twice as sensitive to change of various factors such as solar constant, CO2 content, O3 content, and cloudiness than that of the one with a fixed relative humidity.
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The effect of solar radiation variations on the climate of the Earth

M. I. Budyko
- 01 Oct 1969 - 
TL;DR: In this article, the influence of long-term changes of radiation caused by variations of atmospheric transparency on the thermal regime is studied, and it is found that comparatively small variations in atmospheric transparency could be sufficient for the development of quaternary glaciations.
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Carbon Dioxide Exchange Between Atmosphere and Ocean and the Question of an Increase of Atmospheric CO2 during the Past Decades

TL;DR: In this article, the average lifetime of a CO 2 molecule in the atmosphere before it is dissolved into the sea is of the order of 10 years, which means that most of the CO 2 released by artificial fuel combustion since the beginning of the industrial revolution must have been absorbed by the oceans and that the increase of atmospheric CO 2 from this cause is at present small but may become significant during future decades if industrial fuel combustion continues to rise exponentially.