A prominent climate scientist says it is reasonable to conclude that global warming has caused the unusually snowy weather in the eastern
Dr. Mark Serreze, director of the National Snow and Ice Data Center (NSIDC), a federally-supported research unit at the University of Colorado, told CNSNews.com that the hypothesis is that the decline in Arctic sea ice in recent years has created more open water in the Arctic in summertime, and that this open water absorbs more heat during the summer than the former icepack did, then releases that heat during the winter months, warming the Arctic itself, while pushing cold Arctic air down over the eastern United States and Europe.
“Here’s what happens and here’s what a lot of people get really screwed up on, and it’s straightforward,” Serreze told CNSNews.com. “All right, so it’s getting warmer, and what is happening is that we’re not growing as much ice in winter as we used to be, but we’re melting a heck of a lot more in the summer than we used to.
“So, now what happens is that if we look at the end of summer, end of the melt season in the Arctic—September, say, specifically September--what you find is that there’s much, much more open water than there used to be,” said Serreze. “But what has happened is because that open water is very dark it’s been absorbing a lot of solar heat through the summer."
“So now you’ve got this ocean with all this heat in it that it didn’t used to have. Autumn comes, the sun sets in the
“So you say it’s related to the ice melt. Yes, it is,” said Serreze. “But actually there’s a seasonal lag to it. It’s actually, the ice is melting in summer, exposing all this dark open ocean, picking up all this heat, and, then, autumn comes, the sun sets, that heat’s got to go back to the atmosphere, and that’s what it does. And that greatly warms up the Arctic relative to where it used to be--in other words, relative to, say, where we were 30 years ago. And what’s happening is that that is starting to change the sort of basic temperature gradients in the atmosphere that I talked about before.
“And so if you do that, the thinking is that could actually let this cold air in the Arctic kind of start to spill south,” said Serreze. “Now you say, ‘Well, hasn’t the air been warmed?’ Yes, it has, but it’s still cold air, though.
“But that’s the thinking,” Serreze explained. “The thinking is that, to put it in another way, we’ve put now a heat source in the
“I mean that’s basically it in a nutshell,” said Serreze.
Serreze, whose team monitors the amount of sea ice present in the
NSIDC scientists use data from the National Aeronautics and Space Administration (NASA) to measure how many square miles of sea ice are present in the
In their analysis of the Arctic sea ice extent for January 2001, which was posted on February 2, the scientists said there was an average of only 5.23 million square miles of ice covering the
The NSIDC analysis of January’s Arctic sea ice includes a section titled, “Potential links with mid-latitude weather.” The analysis explores the idea that the diminished Arctic ice cover has contributed to colder, snowier winters in
“Cold air is denser than warmer air, so it sits closer to the surface,” NSIDC says in its analysis. “Around the North Pole, this dense cold air causes a circular wind pattern called the polar vortex , which helps keep cold air trapped near the poles. When sea ice has not formed during autumn and winter, heat from the ocean escapes and warms the atmosphere. This may weaken the polar vortex and allow air to spill out of the
“For example, the last two winters over the East have been cold and snowy,” explained Serreze. “So what happens there? Well, what you’re looking at is some kind of change in the atmospheric circulation, that basically you’ve got this cold, Arctic air plunging down—clearly, because that’s exactly what’s happening—and that gives you a temperature contrast and that’s what gives you the storms, okay?” Serreze said.
“So this all kind of fits together,” said Serreze.
CNSNews.com asked Serreze, “I was hoping you could sort of unpack it for me in terms of: We’re linking global warming to a smaller ice cap to this air being forced … into the mid-latitudes? Is that an accurate characterization?”
“Well, yeah, I think it’s reasonable,” said Serreze.
“The question being asked here: Is there something about the weather that—this crazy winter weather that you’re getting here--that might be kind of forced by something?” said Serreze. “Is there something out there that’s changing, that might actually force the big-scale weather pattern to give you that cold stuff out in the Northeast? And this is where this Arctic stuff comes in, what’s happening in the
Serreze stressed that the idea that Arctic warming was causing winter storms in the mid-latitudes was as yet a theory not a proven fact.
“Now saying this, (I’ve) got to stress here that there is no real smoking gun here yet,” he said. “There’s some physical reasoning behind this as I’ve talked about. There’s evidence from climate models that such a thing can happen. There’s some limited observational evidence for it, okay. But no one has the answer yet, and this is very, very much in sort of a—you know, it’s cutting edge stuff.
“No one really knows for sure, and so we really need to look at this problem a lot harder and we need to see what’s, is this pattern going to continue, this funny winter pattern,” he said. “Are we going to see it next year?
“Those are the sort of questions we’re asking,” he said.
“Maybe this is a transient thing that we’re seeing,” he said. “Maybe it’s that at the state of the sea ice cover we see now, this is the response of the atmosphere. Maybe 20 years down the road, it changes. We don’t know. In other words, what I’m saying, just getting rid of more ice doesn’t mean that winters in
“But it could?” CNSNews.com asked.
“Well, yeah, I mean as a scientist, of course, we're very circumspect about these sorts of things and love to couch these things in uncertainty because these are the things we damn well don’t know.”
You can listen to the full CNSNews.com interview with Dr. Mark Serreze here: