Webberweather53
Meteorologist
Can you go into further detail, I’m trying to learn how things interact at H5 better, it’s my weakness esp vort charts which isn’t good because it’s the blueprint for everything that happens below.
Essentially what's happening is the northern stream disturbance effectively acts to "kick" our southern stream wave faster out to the east despite the fact that they partially phase. As the northern stream backs off more, this allows our main s/w to consolidate more effectively and cut-off from the main streamflow. I mean if you really think about it how many times do we look to shortwaves on the west coast (like last week for ex) wanting a wave to dig and get out and separate itself from the main streamflow. Similarly here, the longer this wave is left alone, the more apt it is to slow down and not get "kicked" by the northern stream wave, and thus it has more space to amplify, and tilt which will ultimately result in a January 2000 solution if the models keep trending towards a slower northern stream wave. I can't believe I was so oblivious to this earlier...