High Resolution Polar Night Vortex Simulation

This new simulation of the stratospheric polar night vortex breakdown was
computed at a significantly higher resolution than the previous one (two to
four times the horizontal and vertical resolution).The breakdown of the
Stratospheric Polar Night Vortex is an atmospheric event that occurs once or
twice each year in the polar wintertime stratosphere. As the polar vortex is
formed, sharp gradients of potential vorticity at the vortex edge isolate polar
air from the air at lower latitudes, producing conditions favorable for
wintertime polar ozone depletion. Rossby waves propagating upward from the
troposphere along the edge of the Polar Vortex grows exponentially in
amplitude, eventually tearing the vortex apart.

This is the second Polar Vortex simulation produced with SEAM. This new
simulation was computed at a significantly higher resolution than the previous
(two to four times the horizontal and vertical resolution), indicating that the
numerical solution of the dynamics has converged in regard to its essential
features.