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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Bibliographic Details
Published in:	Journal of Geophysical Research: Solid Earth Vol. 112; no. B2
Main Authors:	Staiger, Jane, Gosse, John, Toracinta, Rick, Oglesby, Bob, Fastook, James, Johnson, Jesse V.
Format:	Journal Article
Language:	English
Published:	Washington, DC Blackwell Publishing Ltd 01.02.2007 American Geophysical Union
Subjects:	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
Online Access:	Get full text
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