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- W1997118045 endingPage "058101" @default.
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- W1997118045 abstract "After the presence of ionized layers in the Earth's atmosphere was inferred, it took 50 years to quantitatively understand them. The electron density could not be accounted for until Sir David Bates first suggested (along with Sir Harrie Massey) that the main electron-loss process was dissociative recombination with molecular ions, and he and colleagues then developed a theory to predict those rates of dissociative recombination. However, electron impact processes, particularly excitation, have been considered insignificant in most situations, in both planetary and cometary atmospheres. Here we describe cases where recent calculations have shown that electron impact excitation of molecules is important, suggesting that, just as in the time of Sir David Bates, electron-driven processes remain fundamental to our quantitative understanding of atmospheric and cometary phenomena." @default.
- W1997118045 created "2016-06-24" @default.
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- W1997118045 date "2009-10-05" @default.
- W1997118045 modified "2023-10-16" @default.
- W1997118045 title "On the role of electron-driven processes in planetary atmospheres and comets" @default.
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- W1997118045 doi "https://doi.org/10.1088/0031-8949/80/05/058101" @default.
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