Winter of 2013-2014 Sees Most Extreme Dipole on Record: How a Strong Emerging El Nino Conspired With Climate Change to Ignite Record Drought in California and Collapse the Polar Vortex

Dipole. It’s a word often used among meteorologists and climate scientists. But what does it mean?

In weather terms we can simply think of it as this: one side hot, one side cold. So, as a basic principle, it’s pretty direct. But in a world where extremes between hot and cold are becoming more intense, in North America which has just experienced its most extreme dipole anomaly since record keeping began in 1960, it’s also something that’s important to understand as it relates to ongoing human-caused climate change.

For a recent blockbuster scientific paper by Dr. Simon Wang and associates and published in Geophysical Research Letters has now linked this extreme temperature differential, related polar vortex collapse events, and the California drought with both ongoing physical changes to the Earth System due to human caused climate change and to the first rumblings of a monster El Nino in the Pacific.

Envisioning a Dipole Pushed into An Extreme Form by Climate Change

But to understand how an excessively extreme dipole relates to the historic events of the winter of 2013-2014, it helps to open up one’s imagination. It helps to describe the ground-breaking information provided by Dr. Wang’s new paper in descriptive terms. It helps to, at first, envision a wave. Then to imagine the up-slope of the wave forming a hot, red shape. Now imagine the down-slope forming a cold, blue shape. Now think of this wave growing more intense, extending further in both its up-slope and in its down-slope. Growing hotter on the up-slope side and comparatively colder on the down-slope side.

Polar Vortex Collapse January 19

(GFS Model summary of Polar Vortex Collapse event on January 19, 2014 shows 850 mb temperatures over the Eastern US colder than the same temperatures over parts of Greenland and the Arctic Ocean. 850 mb temperatures over St. Augustine, FL are the same as 850 mb temperatures over central Greenland. Anomalies on the hot side of the dipole in the Arctic hit +40 degrees Fahrenheit in some places.  Anomalies on the cold side of the dipole hit more than -35 degrees F in some places. Note the twin, dense high pressure systems sitting sentinel just off the California Coast and deflecting storms north into Alaska. Image source: NOAA/GFS.)

Having established the wave form and related temperature extremes, lay the shape over North America and adjacent Pacific Ocean. The up-slope covers the Eastern Pacific, Alaska, a section of the Beaufort Sea in the Arctic, Western Canada and the Western US. The down-slope swings from the eastern side of the Beaufort, on in through Central and Eastern Canada and bisects the US diagonally from the Dakotas to the Gulf Coast east of Texas.

Now let’s envision this wave as a flow of upper level air called the Jet Stream and let’s think about the various atmospheric aspects that feed it. Looking west, we happen upon a very warm pool of water in the Western Pacific east of the Philippines. This warm pool is the source of an El Nino that will likely occur within one years time. A heat pocket given added intensity by both rising atmospheric temperatures and strong winds transferring that added energy into the vast Pacific Ocean. The heat waits, wanting to spread out across the Pacific surface in an energetic return to the air. But, for now, it simmers in its deep pool, providing energy for the powerful dipole we’ve just described.

The heat from this warm pool radiates into the atmosphere creating lift. Further north, a cold pocket is driven south by another strong atmospheric wave pattern over the Asian continent. The cold air pocket runs south over Japan. The hot and the cold difference generates a very strong upper level synoptic (horizontal form weather patterns stretching more than 1,000 kilometers) wind pattern that stretches all the way across the Pacific Ocean.

The winds run southwest to northeast until they encounter the hot bulge of our already described dipole over the Eastern Pacific near the US west coast and Canada. This warm current turned the already rapid winds due north where they rushed up over Alaska and into a sea ice pack far weaker than in decades past. A sea ice sheet gradually thinning, breaking up, and venting heat from a warming Arctic Ocean below. And so these, already strong, winds were not turned back by the now much weaker cold until they had driven far, far into the Arctic Ocean (and it is here that we must give a hat tip to Dr. Jennifer Francis, who finds her predictions regarding sea ice loss and high amplitude Jet Stream waves again validated).

Polar Vortex Ripped in Half

(Upper level wind pattern on January 23, 2014 shows a polar vortex that has essentially been ripped in half by the warm side of the west coast dipole and the high amplitude Jet Stream wave forming over top of it. Image source: University of Washington.)

Now imagine a strong dome of high pressure forming in the wake of this powerful and ongoing wind flow, sheltered and growing ever stronger on the hot side of the dipole. Imagine it blocking the path of storms, even as it concentrated heat and warmth. Imagine California receiving 1/4 or less of its typical winter rainfall as a result. A most recent and extreme insult to years of drought forcing authorities to ration water in many places.

Now return to that strong wind finally being turned south somewhere in the far, far north, in the Beaufort Sea just south of the North Pole. Then imagine these now cold-laden winds rushing south. Running over Hudson Bay and eastern Canada. Roaring over the Great Lakes and carrying with them a cyclone of cold Arctic air that should have remained in the far north. The polar vortex that should have stayed over places like Svalbard but instead collapsed under the warm wind flow and shifted far south to places like Toronto or Chicago or Detroit or Washington DC.

Now at last imagine another synoptic pattern as the Arctic air of the polar vortex encounters the warmth of the Gulf Stream. This pattern is laden with powerful storms that bomb out over the UK again and again, resulting in the stormiest winter for that island nation in over 200 years.

And here we have the dipole of the winter of 2013 and 2014. A west coast that was hot, hotter than usual all the way from California to the far north of Alaska and an East Coast that from Canada to the Gulf Coast became the repository for cold, cold Arctic air that was shoved south as the polar vortex collapsed down the steep face of the one of the largest and longest lasting Jet Stream waves on record.

(Dr. Francis explains how polar amplification results in higher amplitude Jet Stream wave patterns.)

Dipole. One side hot. One side cold. But, in this case, in the case of the winter of 2013-2014, it’s a historic and anomalous dipole. A freak born of the climate change we’ve caused mixing up with the Pacific Ocean heat of a rising El Nino. A record hot, dry winter for the US West that ignites wildfires in winter and forces the government to ration California water resources. A severe dry spell that closes farms and drives US food prices up by 15%. A record cold, stormy winter in the Eastern US and a series of super-intense storms screaming across the North Atlantic to submerge Somerset and rip massive chunks out of a rocky UK coastline.

This clear picture of a climate-change caused event was this week provided through the groundbreaking new research by Dr. Wang and fellows. These top scientists engaged climate models and analyzed past records to find the culprits of the weather extremes we witnessed during this past winter. And what they found was a very high correlation in the models with the extreme dipole over North America and the Arctic, an oncoming El Nino, and climate change driven impacts.

For not only was this year’s dipole the most extreme on record, it was also likely made far more extreme by an emerging Monster El Nino acting in concert with severe global-warming related reductions in Arctic sea ice cover, increases in Pacific Ocean heat and atmospheric moisture content, and related changes to the upper level air flows of the Northern Hemisphere polar Jet Stream.


Probable Causes of the Abnormal Ridge Accompanying the 2013-2014 California Drought, ENSO Precursor and Anthropogenic Warming Footprint


University of Washington

Read Further Excellent Reporting on the Wang Report Here:

California Drought/Polar Vortex Jet Stream Pattern Linked to Global Warming

Bombshell Study Ties Epic California Drought ‘Frigid East’ To Manmade Climate Change

Large and Growing List of Scientific Studies Linking Human Climate Change to Current Weather Extremes (hat tip to Weather Underground)

Changing the Face of Mother Nature

The Seasonal Atmospheric Response to Projected Sea Ice Loss in the Late 21rst Century

Evidence Linking Arctic Amplification to Extreme Weather in the Mid Latitudes

Influence of Low Arctic Sea Ice Minima on Anomalously Cold Eurasian Winters

Impact of Sea Ice Cover Changes on the Northern Hemisphere Winter Circulation

Impact of Declining Arctic Sea Ice on Winter Snowfall

Large Scale Atmospheric Circulation Changes Associated with the Recent Loss of Arctic Sea Ice

A Link Between Reduced Kara-Barents Sea Ice and Cold Winter Extremes Over Northern Continents

Northern Hemisphere Winter Snow Anomalies

Impact of Projected Future Sea Ice Reduction on Extratropical Storminess and the NAO

Cold Winter Extremes in Northern Continents Linked to Arctic Sea Ice Loss

Precipitation Shifts Over Western North America as a Result of Declining Sea Ice Cover

Disappearing Arctic Sea Ice Reduces Available Water in the American West

Interdecadal Connection Between Arctic Temperature and Summer Precipitation Over the Yangtze River Valley in the CMIP5 Historical Simulations

Potential Impacts of the Arctic on Interannual and Interdecadal Summer Precipitation in China

Influence of Arctic Sea Ice on European Summer Precipitation

On the Relationship Between Winter Sea Ice and Summer Atmospheric Circulation over Eurasia

(Partial list, view the rest here)




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