A quasi-permeable barrier in the equatorial lower stratosphere

Mathematics – Logic

Scientific paper

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Meteorology And Atmospheric Dynamics: Middle Atmosphere Dynamics

Scientific paper

Analyses of global isentropic maps of potential vorticity from the United Kingdom Meteorological Office data assimilation system reveal that there is a region of strong meridional potential vorticity gradients in the equatorial lower stratosphere. A semi-Lagrangian tracer transport model is used to show that this region of strong PV gradients acts as a quasi-permeable barrier to cross-equator mass exchange on isentropic surfaces.

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