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And it is this same deflection of the vortex that brings unusually warm air from the south up to the north, so the same deflection causes both warming and cooling of weather, right? That's what the video that SC linked to shows, which is the answer to the question that I earlier posed, yes?Something the Dog Said wrote:
No you are not understanding my explanation of the stratospheric phenomenon warming event. I will see if I can dumb it down even more. There is credible evidence that the warming of the Arctic creates a high pressure system that is causing weakening of the Polar Vortex, which causes deflection of the jet stream downward so that the polar cold pushes downward over North America. I tried to type slowly so maybe you can understand this time.Something the Dog Said wrote:
So if I am understanding you correctly, what you are saying is a warmer climate produces colder weather, as well as warmer weather, as well as more and stronger storms, as well as fewer and weaker storms, and less ice in at the northern pole and more ice at the southern one. Maybe global warming was responsible for the severe winter when Washington was camped at Valley Forge as well?PrintSmith wrote: the Polar Vortex is actually the jet stream encircling the Arctic which keeps the arctic cold in place . The deflection of the jet stream downward is allowing the Arctic Cold to move downward across North America. This is also referred to as a "stratospheric phenomenon warming event" although that sounds counter intuitive. The deflection of the jet stream (weakening of the Vortex) releases that arctic cold downward over North America. The physics of this action is complex and not fully understood as yet, but the evidence is that as the polar ice cap warms, high pressure builds over the Arctic which weakens the polar jet stream allowing it to deflect downward over North America. At the same time the mid Atlantic jet stream is being strengthened by the warming of the oceans to interact with the deflected Polar Vortex in creating the recent cold weather.
Unfortunately, this portends even further cold weather for North America.
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This weather now serves as the backdrop—and perhaps, as the inspiration—for an increasingly epic debate within the field of climate research. You see, one climate researcher, Jennifer Francis of Rutgers University, has advanced an influential theory suggesting that winters like this one may be growing more likely to occur.
And yet in a letter to the journal Science last week, five leading climate scientists—mainstream researchers who accept a number of other ideas about how global warming is changing the weather, from worsening heat waves to driving heavier rainfall—strongly contested Francis's jet stream claim, calling it "interesting" but contending that "alternative observational analyses and simulations have not confirmed the hypothesis." One of the authors was the highly influential climate researcher Kevin Trenberth of the National Center for Atmospheric Research, who also appeared on Inquiring Minds this week alongside Francis to debate the matter.
"I applaud Jennifer for raising the issue," Trenberth said on the show, but he argued that much more research is needed,
That's How Science Works
Stepping back and surveying this exchange, what one sees is a model of how science works when it is working well, in the way that it is supposed to. It's the utter opposite of politicized "debates" in which skeptics go to the media to raise issues that are red herrings or already resolved by researchers, and most scientists don't even bother to respond.
So what happens now? Well, every year is more data, which means that every year is an additional scientific test for Francis.
[youtube:2musxqd5][/youtube:2musxqd5]You can watch Francis give a more thorough scientific explanation of the idea here, complete with an impressive video animation of the jet stream:
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