I would characterize the interplay between the vortex near the Aleutians, the poleward extending EPO ridge, and the TPV lobe(s) collectively as a block. It seems to get kicked off by a cyclonic wave break out of the Aleutian vortex that pinches off the Pac ridge and amps it up into the EPO space, followed by a poleward anticyclonic wave break, which sends the TPV lobe south, and then it all becomes self sustained. Loading the h5 vorticity panel and hitting play is fun stuff. Turbulent flow on the largest scale.