The same process is still at work nowadays](discussion: p. 7) «Yes,
the outgassing process is still operative today because the laws of physics did not suddenly decide to change.»
Yes,
the outgassing process is still operative today because the laws of physics did not suddenly decide to change.
Not exact matches
Atmospheric carbon dioxide derives from multiple natural sources including volcanic
outgassing, the combustion of organic matter, and the respiration
processes of living aerobic organisms; man - made sources of carbon dioxide come mainly from the burning of various fossil fuels for power generation and transport use.
Further calculations by Catling and his team conclude that no abiotic methane sources on a rocky planet could produce enough of the gas to counteract this
process — whether it is volcanic
outgassing from a planet's interior, chemical reactions in hydrothermal vents, even asteroid impacts.
«We've got a spacecraft on the way to Ceres, so we don't have to wait long before getting more context on this intriguing result, right from the source itself,» said Carol Raymond, the deputy principal investigator for Dawn at NASA's Jet Propulsion Laboratory in Pasadena, Calif. «Dawn will map the geology and chemistry of the surface in high resolution, revealing the
processes that drive the
outgassing activity.»
Melting permafrost
outgasses CO2 and methane, and the decrease in sea ice allows oceanic CO2 to mix back into the atmosphere; taken together, these
processes greatly amplify the effect of increased sunlight, driving a relatively rapid exodus from the ice age.
CO2 (ocean
outgassing etc) is an effect, possibly a positive feedback but remember that a positive feedback still acts positively when the initial
process reverses.
I spent years in semiconductor
processing using ultra-high vacuum equipment and the concept of
outgassing is crucial to every aspect of growth.
Some of that will be due to the physical ocean
outgassing and of course some of that is due to biotic
processes.
«All these
processes give a taste of the complex interaction between sea ice, biological productivity, and deep water upwelling as mechanisms controlling CO2
outgassing in the Southern Ocean, particularly at the Antarctic Polar Front, where they are strongly coupled.»