Difference between revisions of "Human earth shapers/ETHS101/Earthsystems/Atmosphere"
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Scientist divide the atmosphere into spheres that encircle the Earth based on composition and temperature | Scientist divide the atmosphere into spheres that encircle the Earth based on composition and temperature | ||
[[File:Atmosphere-layers.jpg|centre|800px|httos://Geo.arc.nasa.gov]] | [[File:Atmosphere-layers.jpg|centre|800px|httos://Geo.arc.nasa.gov]] | ||
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| + | *Most (75%) of the mass of the atmosphere is in the troposphere. | ||
| + | *Mass is about 5.14 x 1018 kg (=514,000,000,000,000,000 kg*) | ||
| + | **estimate from Trenberth & Guillemot, 1994 Total mass of the atmosphere, Journal of Geophysical Research, 99, 23,079-23,088 | ||
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| + | ===Atmosphere on the move=== | ||
| + | [[File:Atmospheric circulation.svg.png|Frame|right|320px|verall circulation of the atmosphere. Known and exploited by sailors. Note the north and south of the equator divide]]Rotation of the Earth, heat from the sun and cooling where there is no sun all help create the circulation systems that move the Earth’s atmosphere. | ||
Revision as of 03:31, 28 March 2019
Atmosphere
Early life began to change the atmosphere by using gases such as methane, sulfur dioxide, and carbon dioxide and expelling oxygen.
The Earth’s atmosphere has evolved with life so now the atmosphere is nearly 21% oxygen. In comparison CO2 in the atmosphere is tiny (0.04%) and methane makes up even less (0.00018%). None of these volume estimates take water vapour into account.
Atmosphere sections
Scientist divide the atmosphere into spheres that encircle the Earth based on composition and temperature
- Most (75%) of the mass of the atmosphere is in the troposphere.
- Mass is about 5.14 x 1018 kg (=514,000,000,000,000,000 kg*)
- estimate from Trenberth & Guillemot, 1994 Total mass of the atmosphere, Journal of Geophysical Research, 99, 23,079-23,088