Extreme cold air outbreak 24 years ago

I went through a list of the most extreme cold air outbreaks in the last few decades today, and found this one:

Satellite image from 03:22 on 13 March 1992, downloaded from the Dundee Satellite Receiving Station

It might be just me, but I thought this one was particularly beautiful, with prettym uch the whole Norwegian Sea covered by polar lows. This was the third most extreme such outbreak in the period after 1979, at least according to the ERA-Interim reanalysis.

Polar low north of Svalbard

In a warming Arctic, things have changed and are going to change even more in the future. Check out this polar low north of Svalbard one year ago:


No sea ice north of Svalbard in January is unusual in itself, but a polar low to top it off? That’s pretty amazing.

There’s also a new paper out by Elizaveta Zabolotskikh et al.: New areas of polar lows over the Arctic as a result of the decrease in sea ice extent. The title speaks for itself, and their argument is that “new areas of open water appear where mesocyclones can arise”.

The thing is that polar lows can’t form over sea ice, so when the sea ice retreats, new ocean areas with relatively warm water are exposed to cold air outbreaks, just the environment that is most favourable for polar low formation.

One of the consequences is that the Kara Sea (east of Novaya Zemlya) suddenly also becomes prone to polar lows, and this is bad news because this is along the Northern Sea Route (which allows ships to travel from Asia to Europe way faster than through the Suez Canal).

This winter is not much better in terms of “missing” sea ice. Here’s an image from the National Snow and Ice Data Center in the US:


There is little doubt that polar lows can form further north than they usually do, and there is also little doubt that this is a portent of things to come.

Multiple polar lows over the Barents Sea

At least three, maybe even four, polar lows were active over the Barents Sea last night. Here’s a nice satellite image taken early Monday morning:

Uten navn 2
Satellite image downloaded from yr.no

All of these are in the category of cyclones known as “comma clouds”, obviously because they look like inverted commas. As a side-note, maybe they should rather be called “apostrophe clouds”. Anyway, they are what we call baroclinic. That means that the low near the surface is linked to a trough higher up in the atmosphere, and these are not located on top of each other. This vertical structure allows the two lows to work together and to strengthen each other.

For more about this interesting mechanism, check out the Norwegian cyclone model, which was developed by the Bergen school of meteorology.

Most polar lows start out as baroclinic, but many of the develop a warm core and gradually enter a phase where they go from baroclinic to barotropic. Then the lows aloft and near the surface are locked in phase and no longer help each other grow. For the polar low to intensify in this stage, it needs to get its energy from the warm ocean surface.

This is how tropical cyclones (hurricanes) get their energy, too, and some polar lows are in certain ways similar to hurricanes. But so far all the research that has been done on “arctic hurricanes” has shown that the ocean surface is far too cold in the Arctic. In fact, we have a paper in review right now where we look at one such polar low.

Here’s another nice image of the current polar lows:

Uten navn 3
Satellite image taken at 18:27 GMT on 13 December 2015, downloaded from the Dundee satellite receiving station

Clouds marching past

The cold air outbreak that I wrote about a few days ago will hit the UK tomorrow (Sunday), with subzero temperatures as far south as London. Here’s a picture of the cold air on its way southwards, taken from Bergen today:


The tall clouds are “mild” Cumulonimbus clouds forming as the moist, warm air over the sea surface rises in the cold air from the Arctic. I remember seeing such clouds, albeit more vigorous ones, during the IPY-THORPEX polar low field campaign in Andøya in northern Norway in March 2008.

Polar low brewing outside northern Norway

I just got an alert from the excellent BarentsWatch site about a polar low off the coast of northern Norway. Here’s the latest satellite image (downloaded from yr.no):


You can clearly see the dual system between Iceland and Norway, and what’s nice about this is that we also see the edge of the cold air outbreak stretching west from the polar lows. Here are some satellite-based wind speeds from about 1600 GMT yesterday, taken from this site:


This shows nicely how strong the winds are along the edge of the outbreak.

Update: I just found winds from this morning, too, and here wind speeds of more than 50 knots (Force 10 on the Beaufort wind force scale) were estimated by the satellite:


That’s pretty hefty. We can trace the development back to the disturbance seen in this picture from Wednesday, a few hours before the wind snapshot above:


It’s moving slowly, but seems to have built some strength since yesterday.

First polar low of 2015/16 season

Our good friend at the Norwegian Met Office in Tromsø, Gunnar Noer, just told me that they observed the first polar low (with an impact on Norway) this season a few days ago. Here’s a satellite image taken at 18:21 on 26 October 2015:


The polar low is clearly visible just north of northern Norway. At 20:00 UTC the polar low is more developed:


It’s also clear that the polar low formed in a cold air outbreak well north of the well polar front (the region that separates cold air in the north from warm air in the south), which is one of the main characteristics of polar lows.

I also found an image of satellite-derived surface wind speeds from the ASCAR radar (click image for higher resolution):


This shows that the polar low produced fairly strong winds. There’s plenty of other interesting features as well (as in pretty much every satellite image):

  • A jet along the sea ice edge just north of Iceland, probably due to the high mountains of Greenland. It’s more common to get jets in northerly flow in this region.
  • The left-side jet off the northern tip of Novaya Zemlya, also due to topography. Left-side jets are normally stronger than right-side jets because flow towards a barrier creates a small-scale high pressure anomaly in front of the barrier, and this strengthens the jet.
  • The strong southerly flow along the coast north of southern Norway, also a left-side jet.
  • The strong winds along the polar front, which isn’t unusual in any way.