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What is the process that creates a tropopause fold? Do these features have any significant impact(s) on weather patterns or the atmosphere?

Cross Section of a Tropopause Fold

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    $\begingroup$ This one is on my list to take a crack at once I dust off my graduate synoptic class notes. $\endgroup$ – casey Apr 17 '14 at 16:06
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I am not not an expert in meteorology, but do study the chemistry involved in these types of events. My understanding is that the folds in the tropopause generally occur below the front of the jet stream, when the potential vorticity is strong enough to transport stratospheric air down through the tropopause/inversion.

Please see the relevant quote from Q. J. R. Meteorol. Soc. (2004), 130, pp. 1195–1212 doi: 10.1256/qj.03.21 Convective mixing in a tropopause fold By H. J. REID and G. VAUGHAN∗ Institute of Mathematical and Physical Sciences, University of Wales, Aberystwyth, UK

"Mixing between stratospheric and tropospheric air can occur most readily in deep intrusions of stratospheric air into the troposphere, such as tropopause folds (Danielsen 1968). They occur because of the ageostrophic circulation at the jet entrance (Hoskins 1982) and coincide with the frontal zone beneath the jet. Deep folds can extend down to the top of the boundary layer (Browell et al. 1987; Vaughan et al. 1994), while smaller folds, extending only into the upper troposphere, are ubiquitous around the polar jet stream (e.g. Vaughan et al. 2001). They also occur beneath the subtropical jet stream (Gouget et al. 1996), where it has been suggested that mixing between the subtropical fold and tropospheric air promotes the generation of new aerosol particles (Zahn et al. 2000). Turbulence within folds can result from shear instability beneath the jet (Pepler et al. 1998; Hartjenstein 2000) or from convection extending up from the boundary layer (Browning and Reynolds 1994)."

As for synoptic scale weather, I don't think a tropopause fold affects the synoptic scale weather events much, but are rather a part of the weather events. The downward mixing of stratospheric air will introduce drier air, leading to lower humidity in the general vicinity. Of course, ozone will be entrained into the tropopause as well, which has air quality implications. And there are certainly feedbacks in the fold phenomena that will affect heat, radiation, and kinetic patterns... but the synoptic weather in the region is going to be more driven by the jet stream itself rather than a fold that may occur. A meteorologist, though, might have better information on that.

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  • $\begingroup$ tropopause folds do impact the meso scale weather. I will come up with another answer shortly. $\endgroup$ – gansub Jan 23 '16 at 6:59
  • $\begingroup$ such events are driven by STE - earthscience.stackexchange.com/questions/2771/…. Think of it as a vacuum pump. High PV streams cause the isoentropes to be sucked upwards (increasing updrafts) and leading to decrease in static stability and increased precipitation. The scale is the issue. High PV streams affect only affect mesoscale events. $\endgroup$ – gansub Jan 23 '16 at 7:22
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Cross tropopause transport seems to be the main driver : Take a look at this.

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    $\begingroup$ Can you summarize what is in that presentation that supports your answer as well as develop your answer a bit more than a single sentence? We like our answers to stand on their own even if that link is someday removed. $\endgroup$ – casey May 2 '14 at 12:50

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