“…at locations of the broader, weaker, westward jets). It is interesting to note that these regions at the westward jet peaks have been interpreted as latitudes where the atmosphere violates Arnol'd's second stability theorem (Read et al, 2009), possibly leading to significant eddy activity in these locations (waves, large vortices, the hexagon and the ribbon wave, etc.). It would also appear that these regions exhibit the most rapid atmospheric response to seasonal insolation changes in the troposphere.…”