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The natural greenhouse effect of atmospheric oxygen (O2) and nitrogen (N2)
Karlsruhe Institute of Technology.
Luleå tekniska universitet, Institutionen för system- och rymdteknik, Rymdteknik.ORCID-id: 0000-0002-4478-2185
Luleå tekniska universitet, Institutionen för system- och rymdteknik, Rymdteknik.ORCID-id: 0000-0001-6389-1160
Karlsruhe Institute of Technology.
Vise andre og tillknytning
2012 (engelsk)Inngår i: Geophysical Research Letters, ISSN 0094-8276, E-ISSN 1944-8007, Vol. 39, s. L10706-Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

The effect of collision-induced absorption by molecular oxygen (O 2) and nitrogen (N 2) on the outgoing longwave radiation (OLR) of the Earth's atmosphere has been quantified. We have found that on global average under clear-sky conditions the OLR is reduced due to O 2 by 0.11 Wm -2 and due to N 2 by 0.17 Wm -2. Together this amounts to 15% of the OLR-reduction caused by CH 4 at present atmospheric concentrations. Over Antarctica the combined effect of O 2 and N 2 increases on average to about 38% of CH 4 with single values reaching up to 80%. This is explained by less interference of H 2O spectral bands on the absorption features of O 2 and N 2 for dry atmospheric conditions

sted, utgiver, år, opplag, sider
2012. Vol. 39, s. L10706-
HSV kategori
Forskningsprogram
Rymdteknik
Identifikatorer
URN: urn:nbn:se:ltu:diva-13944DOI: 10.1029/2012GL051409ISI: 000304561000002Scopus ID: 2-s2.0-84861685040Lokal ID: d43254cd-c524-428e-a24a-72664bd0a3d6OAI: oai:DiVA.org:ltu-13944DiVA, id: diva2:986897
Merknad
Validerad; 2012; Bibliografisk uppgift: Article number L10706; 20120612 (ysko)Tilgjengelig fra: 2016-09-29 Laget: 2016-09-29 Sist oppdatert: 2018-07-10bibliografisk kontrollert

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