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...

Celý popis

Uloženo v:

Podrobná bibliografie
Vydáno v:	Journal of Geophysical Research: Solid Earth Ročník 112; číslo B2
Hlavní autoři:	Staiger, Jane, Gosse, John, Toracinta, Rick, Oglesby, Bob, Fastook, James, Johnson, Jesse V.
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Washington, DC Blackwell Publishing Ltd 01.02.2007 American Geophysical Union
Témata:	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 přístup:	Získat plný text
Tagy:	Přidat tag Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!

Buďte první, kdo okomentuje tento záznam!