Cooling of Atmosphere Due to CO2 Emission

  title={Cooling of Atmosphere Due to CO2 Emission},
  author={George Varos Chilingar and Leonid F. Khilyuk and Oleg G. Sorokhtin},
  journal={Energy Sources, Part A: Recovery, Utilization, and Environmental Effects},
  pages={1 - 9}
Abstract The writers investigated the effect of CO2 emission on the temperature of atmosphere. Computations based on the adiabatic theory of greenhouse effect show that increasing CO2 concentration in the atmosphere results in cooling rather than warming of the Earth's atmosphere. 

The Influence of the Atmospheric Transmission for the Solar Radiation and Earth's Surface Radiation on the Earth's Climate

The physical and mathematical model of the planetary heat balance is developed and it is shown the possibility of the decreas- ing of the atmospheric and surface temperatures with the decreasing of the Atmospheric Transmission for IR spectrum range, and this decreasing can’t be equilibrated with the change of the atmosphere for the incoming solar radiation.

Modeling of the Earth's Planetary Heat Balance with Electrical Circuit Analogy

The integral heat model for the system of the Earth’s surface—the atmosphere—the open space based on the electrical circuit analogy is presented. Mathematical models of the heat balance for this

A Nexus between Carbon Emissions and Land Surface Temperature in the Six Ecological Zones of Nigeria

The increase in the emission of carbon dioxide (CO2) in the atmosphere has been identified as a driving cause of global climate change which is a threat to the normal functioning of human and natural

Density of Jatropha curcas Seed Oil and its Methyl Esters: Measurement and Estimations

Density data as a function of temperature have been measured for Jatropha curcas seed oil, as well as biodiesel jatropha methyl esters at temperatures from above their melting points to 90 °C. The

Sveuciliste u Zagrebu Prirodoslovno-matematicki fakultet Fizicki odsjek

In this paper we describe the use of the ShakeMap software package for creating scenario maps of earthquakes for which we assumed and manually entered the magnitude, location and geometry of the



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

Arrhenius’s paper is the first to quantify the contribution of carbon dioxide to the greenhouse effect (Sections I-IV) and to speculate about whether variations in the atmospheric concentration of

Evolution of the Earth's Global Climate

Abstract The model of the Earth's climate change described here is based on the Earth's global evolution theory and adiabatic theory of the greenhouse effect. The main factor determining climate's

Global warming and long-term climatic changes: a progress report

The authors believe that recent global warming of Earth’s atmosphere is not due to an increase in anthropogenic carbon dioxide emission but rather to long-term global factors. The human contribution

Environmental Effects of Increased Atmospheric Carbon Dioxide

A review of the literature concerning the environmental consequences of increased levels of atmospheric carbon dioxide leads to the conclusion that increases during the 20th century have produced no

The evolution of the Earth.

The formation of this planet and its atmosphere gave rise to life, which shaped the earth's subsequent development. Our future lies in interpreting this geologic past.

Terrestrial ecosystems and the carbon cycle

The terrestrial biosphere plays an important role in the global carbon cycle. In the 1994 Intergovernmental Panel Assessment on Climate Change (IPCC), an effort was made to improve the quantification

On global forces of nature driving the Earth’s climate. Are humans involved?

The authors identify and describe the following global forces of nature driving the Earth’s climate: (1) solar radiation as a dominant external energy supplier to the Earth, (2) outgassing as a major

The Little Ice Age and Medieval Warm Period in the Sargasso Sea

  • L. Keigwin
  • Environmental Science, Geography
  • 1996
Sea surface temperature (SST), salinity, and flux of terrigenous material oscillated on millennial time scales in the Pleistocene North Atlantic, but there are few records of Holocene variability.

Handbook of Geochemistry

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