Sunday, December 10, 2017 2:31:18 PM
upper dynamics: low end jet-stream, 250mb-windspeed/streamlines...
https://www.tropicaltidbits.com/analysis/models/?model=gfs®ion=namer&pkg=uv250&runtime=2017121000&fh=24&xpos=0&ypos=
end of run goes right back to that dual feed system that starts/splits in the pacific @ california for north and south paths.
The south path looks much like that cross mexico flow that kept blowing the cold up and out last year.
but this year, we have that split thing going on...
the north path helps churn that huge (* purple cold patch) (* https://www.netweather.tv/charts-and-data/gfs ) northeast of US "that wasn't there last year ~ it was in siberia" maybe the east will wobble some purple cold down one system after another.
That southern/split flow needs to stay south a tad longer before turning north or the southern split @california needs to stop all together and join the rest of the jetstream
bigger picture
https://www.tropicaltidbits.com/analysis/models/?model=gfs®ion=nhem&pkg=uv250&runtime=2017121000&fh=384
a strong high mexico cross flow is a possible troubling repeat of last year's winter delay
end of run
https://www.tropicaltidbits.com/analysis/models/?model=gfs®ion=namer&pkg=uv250&runtime=2017121000&fh=24&xpos=0&ypos=
end of run goes right back to that dual feed system that starts/splits in the pacific @ california for north and south paths.
The south path looks much like that cross mexico flow that kept blowing the cold up and out last year.
but this year, we have that split thing going on...
the north path helps churn that huge (* purple cold patch) (* https://www.netweather.tv/charts-and-data/gfs ) northeast of US "that wasn't there last year ~ it was in siberia" maybe the east will wobble some purple cold down one system after another.
That southern/split flow needs to stay south a tad longer before turning north or the southern split @california needs to stop all together and join the rest of the jetstream
bigger picture
https://www.tropicaltidbits.com/analysis/models/?model=gfs®ion=nhem&pkg=uv250&runtime=2017121000&fh=384
a strong high mexico cross flow is a possible troubling repeat of last year's winter delay
end of run
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