Atmospheric scaling of cosmogenic nuclide production: Climate effect

Absorption of cosmic rays by atmospheric mass varies temporally due to a redistribution of atmospheric pressure by ice sheets during glaciations, the compression and expansion of the atmosphere due to cooling and warming, and changes in katabatic winds near large ice masses. These atmospheric proces...

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Vydané v:	Journal of Geophysical Research: Solid Earth Ročník 112; číslo B2
Hlavní autori:	Staiger, Jane, Gosse, John, Toracinta, Rick, Oglesby, Bob, Fastook, James, Johnson, Jesse V.
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Washington, DC Blackwell Publishing Ltd 01.02.2007 American Geophysical Union
Predmet:	anthropogenic cosmogenic denudation Earth sciences Earth, ocean, space erosion Exact sciences and technology land use watershed atmosphere altitude models Atmospheric condition absorption ice Katabatic wind expansion atmospheric pressure glaciation ice sheets nunataks Production rate cosmic rays climate effects cooling warming temperature compression calibration
ISSN:	0148-0227, 2156-2202
On-line prístup:	Získať plný text
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