North Pole Region Predicted to Experience Another Instance of Above Freezing Temperatures as the Bering Sea Ice is Blasted Away

Those previously rare instances of above freezing temperatures in the Arctic north during winter time are happening more and more often.

(February 20 NASA satellite imagery shows Bering Sea with mostly open water as highly atypical above freezing temperatures drive far north. Note that patches of open water extend well into the Chukchi Sea. Image source: NASA.)

Just Monday and Tuesday of this week, Cape Jessup, Greenland — a mere 400 miles away from the North Pole — experienced above freezing temperatures for two days in a row. This following a February 5 warm air invasion that drove above 32 F temperatures to within 150 miles of this furthest northerly point in our Hemisphere¬†even as, by February 20th, a warm air invasion relentlessly melted the Bering Sea’s typically frozen surface (see image above).

Far Above Average Temperatures Over Our Pole

It’s not just a case of warming near the pole itself. It’s the entire Arctic region above the 66 degree North Latitude line. Over the past few days, Arctic temperature anomalies have exceeded 6 degrees Celsius above the 1981 to 2010 baseline. A period that was already showing a serious warming trend.

(Insane levels of warmth relentlessly invade the Arctic during February — hammering the sea ice and wrecking havoc on local environments. Image source: Climate Reanalyzer.)

For reference, 6 C warmer than normal daily readings for any large region of the Earth’s surface is a very serious temperature departure. And the Arctic is clearly feeling it as it suffers the lowest sea ice extent in our record keeping. The heat is meanwhile wreaking out of control harm on the Arctic environment — endangering key species like seals, walrus, puffins, and polar bears, setting off very rapid coastal erosion as storm waves grow taller, triggering far more extensive and powerful Arctic wildfires, and causing mass land subsidence and various harmful environmental feedbacks from permafrost thaw. It’s also causing Greenland’s massive glaciers to melt faster — contributing to an acceleration in the rate of global sea level rise.

The warm air has been invading primarily from the ocean zones in the Atlantic and the Pacific. Warm storms have frequently roared north through the Barents Sea and up the Greenland Strait near Svalbard. Massive blocking high pressure systems have shoved outlandishly warm temperatures through the Bering Sea on the Pacific side day after day, month after month.

Warm Air Invasions Clear Sea Ice During Winter

A recent warm air invasion has practically cleared the Bering Sea of ice. And the ice edge there is further withdrawn than it has ever been in its history. As we can see from the below animation, this crazy and rapid clearing of ice continues to drive further and further north — ushered in by a relentless invasion of warm air — during February. A time when Bering ice should be expanding, not contracting.

What’s causing such extreme polar weather? In two words — climate change. But drilling down, the details can actually get pretty complicated.

During recent winters, human-caused climate change has been driving temperatures into never-before-seen ranges over our northern pole. Increasingly, Sudden Stratospheric Warming events have been propelling warm air into the upper layers of the atmosphere. The Polar Vortex, which during winter relies on a column of sequestered cold air to maintain stability, is blown off-kilter as these upper level layers heat up. This, in turn, has generated extreme wave patterns in the winter Northern Hemisphere Jet Stream — enabling much warmer than usual temperatures to rocket northward.

An Ongoing Series of Warming Events

On December 30 of 2015, and enabled by a high amplitude Jet Stream wave, a powerful warm storm event pushed a strong wedge of warm, above freezing, air all the way across the 90 North Latitude line. Meanwhile, Jessup Greenland hit above freezing for what was likely the first time ever over the past two winters. Last year’s Arctic sea ice hit the lowest levels ever seen during March due to all the extra heat. And the warm temperature extremes appear to be deepening.

Now, as of mid February, a powerful Sudden Stratospheric Warming Event has again blown the Polar Vortex off kilter — weakening it and enabling warm air to flood into the Arctic even as colder air is displaced southward over Canada, the Western U.S. and Europe. Translating to the surface, this train wreck in the upper level winds has driven the extreme polar warming events of the past 8-10 days even as cold air invasions have overtaken Europe and the U.S. East experiences record-breaking heat.

The polar warming event is still ongoing. And it is expected to deliver another blow to an Arctic environment that typically experiences -30 degree Celsius temperatures this time of year. For another major warm wind invasion is forecast to drive above freezing temperatures over the North Pole by this weekend. Strong south to north winds along an extreme ridge in the Jet Stream are predicted to push 1-2 C temperatures (or approximately 55 F above average temps) over the North Pole on Saturday and Sunday.

(High amplitude Jet Stream wave predicted to drive North Pole temperatures to above freezing by Sunday. Image source: Earth Nullschool.)

Though rare during December, above freezing temperatures at the North Pole during February are practically unheard of. The period of February through April should be a time of strengthening and thickening ice ahead of melt season. But during 2018 this appears not to be the case. The ice instead, in key regions, is being delivered with serious setbacks which is greatly retarding this year’s typical Arctic Ocean ice formation.

If this most recent polar warming event emerges as predicted, it will provide yet one more powerful blow to an already greatly weakened Arctic sea ice pack during a time of year when extents and areas should be reaching their peak. And that’s bad news for both the Arctic and global environments.

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