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Concentrations of carbon dioxide and other greenhouse gases in the atmosphere have increased since the beginning of the industrial era.
Composition of greenhouse gases in the atmosphere. The remaining gases are often referred to as trace gases, among which are the greenhouse gases, principally carbon dioxide, methane, nitrous oxide, and ozone. On this planet, the atmosphere is about 100 times thinner than Earth. As with the United States, the majority of the world’s emissions result from electricity generation, transportation, and other forms of energy production and use.
Carbon dioxide enters the atmosphere through burning fossil fuels (coal, natural gas, and oil),. The Molecular Greenhouse Gas Composition of the Atmosphere Taking into Account Vertical Variation. A brew of trace gases accounts for the other 0.03 percent, including the greenhouse gases carbon dioxide, methane, nitrous oxide and ozone.
By volume, the dry air in Earth’s atmosphere is about 78.09 percent nitrogen, .95 percent oxygen, and 0.93 percent argon. The water vapor component of the atmosphere varies around the Earth from near zero in the deserts, both hot and cold, to perhaps seven percent in tropical marine environments. Greenhouse gases Water vapor ( H 2O) Carbon dioxide ( CO 2) Methane ( CH 4) Nitrous oxide ( N 2O) Ozone ( O 3) Chlorofluorocarbons (CFCs) Hydrofluorocarbons (includes HCFCs and HFCs).
Of the greenhouse gases, carbon dioxide (CO 2) is the most prominent. There is precise information on the proportions of all gases in the atmosphere except one and that one is water vapor, the overwhelmingly most important greenhouse gas. The average concentration of the greenhouse gases carbon dioxide, methane, and nitrous dioxide has been increasing.
Ozone is concentrated around cities and in the Earth's stratosphere. The permanent gases whose percentages do not change from day to day are nitrogen, oxygen and argon. Methane is emitted during the production and transport of coal, natural gas, and oil.
Mars also has a mostly carbon dioxide atmosphere, with traces of nitrogen, argon, oxygen, carbon monoxide and some other gases. Overview of Greenhouse Gases Carbon dioxide (CO2):. Sources of atmospheric CO 2 include volcanoes, the combustion and decay of organic matter, respiration by aerobic (oxygen-using) organisms, and the burning of fossil fuels, clearing of land, and production of cement by humans.
Besides argon, already mentioned, other noble gases , neon, helium, krypton, and xenon are also present.
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