Synoptic scale weather disturbances tend to form in the regions of
maximum jet stream wind speed and propagate downstream.
Not exact matches
Stronger mid-latitude westerly
wind maxima have occurred in both hemispheres in most seasons from at least 1979 to the late 1990s, and poleward displacements of corresponding Atlantic and southern polar front
jet streams have been documented.
This behavior is expected if there is a baroclinic feedback that encourages the
maximum baroclinic instability to be coincident with the
maximum zonal
wind - speed, and discourages the meridional vacillation of the eddy - driven
jet stream.