Articles | Volume 16, issue 2
Atmos. Chem. Phys., 16, 541–560, 2016
Atmos. Chem. Phys., 16, 541–560, 2016

Research article 19 Jan 2016

Research article | 19 Jan 2016

The tropopause inversion layer in baroclinic life-cycle experiments: the role of diabatic processes

D. Kunkel et al.

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Cited articles

Bell, S. W. and Geller, M. A.: Tropopause inversion layer: seasonal and latitudinal variations and representation in standard radiosonde data and global models, J. Geophys. Res.-Atmos., 113, D05109,, 2008.
Birner, T.: Fine-scale structure of the extratropical tropopause region, J. Geophys. Res., 111, D04104,, 2006.
Birner, T.: Residual Circulation and Tropopause Structure, J. Atmos. Sci., 67, 2582–2600,, 2010.
Birner, T., Dörnbrack, A., and Schumann, U.: How sharp is the tropopause at midlatitudes?, Geophys. Res. Lett., 29, 1700,, 2002.
Birner, T., Sankey, D., and Shepherd, T. G.: The tropopause inversion layer in models and analyses, Geophys. Res. Lett., 33, L14804,, 2006.
Short summary
By conducting various simulations of dry and moist baroclinic life cycles, we aimed to improve the understanding of whether dynamical or diabatic processes are more relevant to form a tropopause inversion layer at midlatitudes. Most importantly, our experiments highlighted the role of different moisture related processes for the formation and evolution of the tropopause inversion layer with varying relevance and strength in different phases of the baroclinic life cycles.
Final-revised paper