A global view of the extratropical tropopause transition layer from Atmospheric Chemistry Experiment Fourier Transform Spectrometer O3, H2O, and CO

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Horizontal water vapor transport in the lower stratosphere from subtropics to high latitudes during boreal summer (2013, background): “, 2002] extending within about 30 K distance of the extratropical local tropopause [Hoor et al., 2004; Hegglin et al., 2009], additional processes may play a role, involving baroclinic instability and convection [e.”
Chemical and dynamical discontinuity at the extratropical tropopause based on START08 and WACCM analyses (2011, background): “This is a different approach complementary to studies investigating the vertical trace gas gradients using the altitude relative to the lapse rate tropopause [Pan et al., 2004; Hegglin et al., 2009; Tilmes et al., 2010].”
THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE (2011, methodology): “This increased Brewer ‐ Dobson circulation implies an increase in ozone in the extratropical LMS [ Shepherd , 2008; Li et al. , 2009; Gettelman et al. , 2010] and in the mass of STE [ Sudo et al. , 2003; Hegglin et al. , 2009].”