A natural response to a decreasing temperature gradient will be a wavier jet - if there is less overall 'velocity' then it will be more prone to large meanders - consider a river: when it has a lot of velocity (mountain stream) it tends to go fairly straight; when it is moving more sluggishly (downstream) you get large meanders, and sometime ox-bow lakes (in the atmosphere, a cut-off low).
Of course, we've seen some large meanders this winter - but it doesn't mean all of the jet is sluggish. Here in the UK we've been sat at the end of a powerful Atlantic jet for most of the winter, and had storm after storm, and quite likely the wettest winter on record.
Ultimately, larger meanders will mean more extreme temperature contrasts between locations and seasons - but there is no guarantee of what side of any meander you might be on in any season! Thus, if a large trough sets up over the western USA in May, and sticks there, you know what that means! But the trough might set-up to the east and stick there.