Current coverage of polar vortex intrusion. ‘Polar vortex’ could send wind chill to 65 below zero in Midwest.

Carson Walker: Temperature records will likely be broken during the short, yet forceful deep freeze that will begin in many places on Sunday and extend into early next week. That’s thanks to a perfect combination of the jet stream, cold surface temperatures and the polar vortex — a counterclockwise-rotating pool of cold, dense air, said Ryan Maue, of Tallahassee, Fla., a meteorologist for Weather Bell. URL

Dennis Lynch: Meteorologists across the nation have pointed to a ‘polar vortex’ as one of the many systems responsible for what is set to be a rare and extreme weather weekend. URL

Here’s What The ‘Polar Vortex’ That’s Hitting The US Actually Is Business Insider ( Jan 5, 2013)

Lauren Friedman: Polar vortexes, though, are nothing new. They occur seasonally at the North Pole, and their formation resembles that of hurricanes in more tropical regions: fast-moving winds build up around a calm center. Unlike a hurricane, these are frigid polar winds, circling the Arctic at more than 100 miles per hour.

The spinning winds typically trap this cold air in the Arctic. But the problem comes when the polar vortex weakens or splits apart, essentially flinging these cold wind patterns out of the Arctic and into our backyards. NOAA scientists have suggested that warming temperatures in the Arctic may be responsible for the weakening of the polar vortex. When the vortex weakens, it’s more likely to break apart and become a factor in our winter weather. URL

Current jet stream and polar vortex configuration

Coldest Air in Decades Clearing Customs, Entering U.S.

Andrew Freedman: The atmospheric blocking, which is not as strong as some other blocking events in recent years, is forcing a large section of the polar vortex to break off and move south out of Central Canada and into the U.S. The polar vortex is an area of cold low pressure that typically circulates around the Arctic during the winter, spreading tentacles of cold southward into Europe, Asia, and North America at times. URL

Andrew Freedman: At the peak of the Arctic outbreak, temperatures may be between 20°F and 40°F below average in large parts of the continental U.S., with dangerous wind chills affecting cities like Minneapolis, Chicago, Cleveland, St. Louis, Washington, D.C., New York, and Boston. The U.S. will have the dubious distinction of experiencing the largest cold temperature anomalies of any land area in the Northern Hemisphere during the height of the biting cold. By comparison, temperatures across Greenland and much of the Arctic will be above average for this time of year, albeit still frigid. URL

Melting Arctic sea ice could be altering jet stream Ars Technica (Dec 2013)

Scott K. Johnson: Qiuhong Tang and Xuejun Zhang, of the Chinese Academy of Sciences, and Jennifer Francis, of Rutgers, decided to look for patterns of atmospheric change correlated with the loss of Arctic summer sea ice and the decline of early summer snow cover. Using reanalyses, which generate global datasets based on all the available measurements, they examined how the lower, middle, and upper troposphere responded to variations in sea ice and snow cover from 1979 (the start of the satellite era) to 2012.

They found modest correlations with the behavior of high-level winds and the differences in atmospheric pressure that drive them, more so for sea ice than snow cover. Over most regions, the average position of the jet stream moved a little northward when summer sea ice was smaller, while the opposite was true for the western edges of continents. The high-level, west-to-east winds of the jet stream also slowed a bit.

Those two factors are consistent with the hypothesized link between sea ice and weather extremes. When the jet stream slows, it gets wigglier, with ponderous meanders extending north and south. Because the temperature difference across the jet stream is so large, these slow-moving excursions can lead to temperature extremes. The early loss of snow cover can exacerbate this, as it means soils can dry out earlier in the summer. Not only does that make a region susceptible to drought, but low soil moisture allows temperatures to rise higher.

Another recent paper published in Environmental Research Letters focused on Northern Europe, using different techniques. There, an unusual run of six wet summers left people wondering if Arctic sea ice loss could have contributed.

Looking through the data, University of Exeter researcher James Screen saw that wet conditions are associated with the jet stream coming south from its average position. Conversely, it’s drier when it stays far to the north. Screen ran two climate model simulations: one in which Arctic sea ice was present at its 1979 extent and one at its diminished 2009 extent. Each simulation was repeated for a century’s worth of summers to calculate the average position of the jet stream over Europe.

Consistent with the study by Tang, Zhang, and Francis, the lower sea ice extent in the model was associated with the jet stream moving a little southward over Europe as part of its amplified “wiggliness.” That brought more precipitation to Northern Europe in the model simulations.

However, Screen emphasizes that these things vary quite a lot from year to year on their own, and the simulated sea ice impact was only a slight shift. “This means that whilst low sea ice coverage increases the risk of wet summers, other factors can easily negate this influence and lead to dry summers during depleted ice conditions or wet summers during extensive ice conditions,” he writes. URL

Arctic warming, jet stream coupling may mean another winter of extreme storms and cold air outbreaks for eastern U.S. Washington Post (Dec 2013)

Steve Tracton: Investigation of differences between northern hemisphere winters from 2001-2013 and 1998-2000 leaves little doubt that a large and consequential trend has occurred in the configuration of the polar jet stream which is linked directly to pronounced warming in high northern latitudes. Moreover, the overall trend has remained largely unbroken and appears to have accelerated in the last six winters.

The coupling between Arctic warming and polar jet is oft referred to as arctic amplification. It features a likely, but not yet definitively proven, link to the apparent increase in extreme, high impact winter weather events occurring over varying regions in mid-to-high latitudes in the northern hemisphere.

It’s critical to note that the seasonal averages examined reflect the net effects of considerable variability of weather systems and processes.  As shown below, the single most prominent signal in the means (averages) to emerge from this variability during the 2000s is one closely resembling the negative phase of the North Atlantic Oscillation (hereafter referred to as -NAO). It is well known that periods of -NAO are favorable for major winter storms affecting the mid-high latitudes from eastern North America though western Europe. Preceding and/or accompanying such storms are surges of anomalous cold penetrating further south over eastern U.S. than nominally expected. URL

Climate Change & The Jet Stream Climate Central (Nov 2013)

Andrew Freedman: Scientists have only recently begun to detect changes in the jet stream that may be tied to global warming. Unraveling the complexities of this emerging scientific research is critical to understanding where our weather is headed.

As the globe continues to warm, it is already having an effect on the jet stream and corresponding weather patterns, according to the latest U.N. IPCC climate report, which states: “It is likely that circulation features have moved poleward since the 1970s, involving a widening of the tropical belt, a poleward shift of storm tracks and jet streams, and a contraction of the northern polar vortex. Evidence is more robust for the Northern Hemisphere.” The research that goes into this statement comes from multiple lines of evidence – from analyses of the expansion of the tropical Hadley Cell to satellite measured outgoing radiation, radiosonde observations, and weather pattern reanalyses. But just as certainty builds for a poleward shifting jet, there still remain questions about whether the jet is amplifying and promoting more blocking patterns. URL

Cold winter in a world of warming? Real Climate (2010)

Rasmus Benestad: One interesting question is how the Barents-Kara sea-ice affects the winter temperatures over the northern continents. By removing the sea-ice, the atmosphere above feels a stronger heating from the ocean, resulting in anomalous warm conditions over the Barent-Kara seas. The local warming gives rise to altered temperature profiles (temperature gradients) along the vertical and horizontal dimensions.

Changes in the temperature profiles, in turn, affect the circulation, triggering a development of a local blocking structure when the sea-ice extent is reduced from 80% to 40%. But Petoukhov and Semenov also found that it brings a different response when the sea-ice is reduced from 100% to 80% or from 40% to1%, and hence a non-linear response. The most intriguing side to this study was the changing character of the atmospheric response to the sea-ice reduction: from a local cyclonic to anti-cyclonic, and back to cyclonic pattern again. These cyclonic and anti-cyclonic patterns bear some resemblance to the positive and negative NAO phases. URL

Related

• DailyKos Polar Vortex, Jet Streams, Stratospheric Warming events, Rossby Waves, and Arctic Blasts (Jan 2014)
• Washington Post Arctic warming, jet stream coupling may mean another winter of extreme storms and cold air outbreaks for eastern U.S. (Dec 2013)
• Climate Central Climate Change & The Jet Stream (Nov 2013)
• DailyKos Sudden Stratospheric Warming Split the Polar Vortex in Two  (Jan 2013)
• Climate Central Stratospheric Phenomenon Is Bringing Frigid Cold to U.S  (Jan 2013)
• ClimateCrocks Arctic Warming Effect on Jet Stream = More Extremes (2012)
• RealClimate Cold winter in a world of warming? (2010)
• Wunderground Weather Extremes Tied to Jet Stream Changes
• Wikipedia Jet stream
• Wikipedia Polar vortex

References