Thursday, 7 June 2001
Using meteorological analyses and shallow water model simulations we
examine the dynamics of Rossby wave breaking on the sub-tropical
tropopause. We focus on wave breaking events that lead to an intrusion
of high potential vorticity (stratospheric) air into the tropical
upper troposphere. The occurrence of these events are shown to be
sensitive to the basic state, and in particular zonal variations in
the flow. This sensitivity results in strong seasonal and inter-annual
(ENSO) variations in the frequency of these intrusions. We also
examine the link between the intrusions and the occurrence of deep
convection. In particular, PV inversion calculations to determine the
vertical motion attributable to the anomalous PV within the intruded
tongues of stratospheric air.
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