Imprints of the upper troposphere and the stratosphere on column-averaged methane

  • Methane is the second most important anthropogenic greenhouse gas and there is renewed strong increase of atmospheric methane since 2007. Although the overall global budget of methane emissions is well constrained, the quantitative attribution to the underlying sources remains an up-to-date open scientific question. The column-averaged dry-air mixing ratio of methane, denoted as XCH4, is a special atmospheric measure attainable only via ground-based and satellite-derived observations. The resulting data enable a global spatiotemporal overview of the atmospheric methane concentrations and, thus, are very suitable for the quantification of methane emission sources by means of inverse modeling. However, even the strongest surface emission fluxes only produce a slight change in the XCH4 signal in relation to the co-resident background level in XCH4. For this reason, an accurate quantification of methane emissions from XCH4 data only is possible, if observations and simulations of XCH4Methane is the second most important anthropogenic greenhouse gas and there is renewed strong increase of atmospheric methane since 2007. Although the overall global budget of methane emissions is well constrained, the quantitative attribution to the underlying sources remains an up-to-date open scientific question. The column-averaged dry-air mixing ratio of methane, denoted as XCH4, is a special atmospheric measure attainable only via ground-based and satellite-derived observations. The resulting data enable a global spatiotemporal overview of the atmospheric methane concentrations and, thus, are very suitable for the quantification of methane emission sources by means of inverse modeling. However, even the strongest surface emission fluxes only produce a slight change in the XCH4 signal in relation to the co-resident background level in XCH4. For this reason, an accurate quantification of methane emissions from XCH4 data only is possible, if observations and simulations of XCH4 achieve high accuracy (<0.3 %). Meeting this standard requires that XCH4 as a vertically integrating measure correctly accounts for the existing methane concentrations of various height layers. Therefore, this work examines the effects of atmosphere dynamical processes in the upper troposphere and the stratosphere on the accuracy of XCH4 observations, and simulations, respectively.show moreshow less

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Metadaten
Author:Andreas Ostler
URN:urn:nbn:de:bvb:384-opus4-40604
Frontdoor URLhttps://opus.bibliothek.uni-augsburg.de/opus4/4060
Advisor:Ralf Sussmann
Type:Doctoral Thesis
Language:English
Publishing Institution:Universität Augsburg
Granting Institution:Universität Augsburg, Fakultät für Angewandte Informatik
Date of final exam:2016/12/19
Release Date:2017/03/16
GND-Keyword:Methanemission; Mittlere Atmosphäre; FT-IR-Spektroskopie; Troposphäre; Stratosphäre
Institutes:Fakultät für Angewandte Informatik
Fakultät für Angewandte Informatik / Institut für Geographie
Dewey Decimal Classification:5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften
Licence (German):Deutsches Urheberrecht mit Print on Demand