• After witnessing the continued decrease of involvement in the SpotterNetwork staff in serving SN members with troubleshooting issues recently, I have unilaterally decided to terminate the relationship between SpotterNetwork's support and Stormtrack. I have witnessed multiple users unable to receive support weeks after initiating help threads on the forum. I find this lack of response from SpotterNetwork officials disappointing and a failure to hold up their end of the agreement that was made years ago, before I took over management of this site. In my opinion, having Stormtrack users sit and wait for so long to receive help on SpotterNetwork issues on the Stormtrack forums reflects poorly not only on SpotterNetwork, but on Stormtrack and (by association) me as well. Since the issue has not been satisfactorily addressed, I no longer wish for the Stormtrack forum to be associated with SpotterNetwork.

    I apologize to those who continue to have issues with the service and continue to see their issues left unaddressed. Please understand that the connection between ST and SN was put in place long before I had any say over it. But now that I am the "captain of this ship," it is within my right (nay, duty) to make adjustments as I see necessary. Ending this relationship is such an adjustment.

    For those who continue to need help, I recommend navigating a web browswer to SpotterNetwork's About page, and seeking the individuals listed on that page for all further inquiries about SpotterNetwork.

    From this moment forward, the SpotterNetwork sub-forum has been hidden/deleted and there will be no assurance that any SpotterNetwork issues brought up in any of Stormtrack's other sub-forums will be addressed. Do not rely on Stormtrack for help with SpotterNetwork issues.

    Sincerely, Jeff D.

Wavier jet stream 'may drive weather shift' ?

Baroclinic instability is directly driven by the temperature gradient, which should be decreasing. You would think the magnitude of waves would decrease, not increase. I do not know what the impact on the planetary wavenumber (and thus in part propagation speed) would be.

However neither of these effects are distinguishable from noise at this point.
 
Articles exactly like this pop up just about every year. I'm not for or against the results of the research... just wanted to state that such conclusions have never been substantiated well and there is not enough evidence to make a clear distinction between whether it's related to climate change or is just natural variability.
 
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.
 
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