First post from me for a VERY long time.
Been following this Strat-thread for a long time now,some very knowledgeable people on here.
Fascinating subject and i,m pleased to see Stratospheric Dynamics being used as a forecasting tool.
About 14 years ago on (Other)weather site......I was very keen to get across the importance of Strat-Dynamics in the overall pattern
of Northern Hemisphere winters.Nobody at the time, gave it much credence(apart from Steve Murr).I think he realized, as I did,that
really, the wintertime polar vortex is the governor.Liken it to a giant flywheel,it gains its energy from the thermal gradient in autumn/winter.Like a flywheel,if you knock it,it will loose energy and slow down,untill it gains MORE energy,and speeds up again.
Keep on knocking it and you will eventually slow it right down......and stop it.
I think the classic events that took place in the Stratophere in December 1962,and Jan/Feb 1963 can be used as a benchmark
in Tropospheric/Stratospheric dynamics.In late December 62,and early Jan 63 the polar vortex was a very cold,almost circumpolar
cyclone.(This ties in with what Chionomaniac was saying about the vortex strength)It seems to me, that the kinetic energy that the votex gains,ultimately, can sometimes lead to its own DISTUCTION.The central temperatures of the votex were near to -85C,with a band of westery winds at 10mb sometimes exceeding 200kt.
The Major Stratopheric Warming then was quite astounding,and explosive.Around the middle of January,10mb temperatures above Edmonton,Alberta.began a rise.Over five days,the temperature rose 67C.The changes in circulation in Jaunuary and February 1963
extended from the Tropopause to at least 55km.
F5