30-Jan-2023: Extremely cold weather in Asia is linked to Polar Vortex

Polar Vortex

  • Refers to an expanse of cold air that circles the Arctic
  • Occasionally shifts south from the North Pole, causing extremely cold weather
  • Vortex: counterclockwise flow of air that keeps colder air near the Poles
  • Exists near poles, weakens in summer, strengthens in winter
  • Lack of consensus, but believed to become more frequent and pronounced with a warming planet

30-Jan-2023: Extremely cold weather in Asia is linked to Polar Vortex

Polar Vortex

  • Refers to an expanse of cold air that circles the Arctic
  • Occasionally shifts south from the North Pole, causing extremely cold weather
  • Vortex: counterclockwise flow of air that keeps colder air near the Poles
  • Exists near poles, weakens in summer, strengthens in winter
  • Lack of consensus, but believed to become more frequent and pronounced with a warming planet

2019

2-Jan-2019: Polar Vortex and its effects on weather patterns

Weather experts are predicting an extremely cold January and February for the northeastern United States, much of northern Europe and parts of Asia. The reason being given is the polar vortex.

In this decade, the polar vortex has also been blamed on extremely cold weather in the United States in 2014 and the infamous ‘Beast from the East’, the blast of cold weather that blew from Siberia towards western Europe and the UK in February and March of 2018.

So what exactly is a polar vortex? A polar vortex is a low pressure area—a wide expanse of swirling cold air—that is parked in polar regions. During winter, the polar vortex at the North Pole expands, sending cold air southward. This happens fairly regularly and is often associated with outbreaks of cold temperatures in the United States. The polar vortex spins in the stratosphere, a layer of the atmosphere 10-48 km above the ground and above the troposphere, where most familiar weather patterns develop.

Usually, when the vortex is strongest, cold air is less-likely to plunge deep into North America or Europe. In other words, it forms a wall that protects the mid-latitudes from cold Arctic air.

Occasionally, the polar vortex is disrupted and weakens, due to wave energy propagating upward from the lower atmosphere. When this happens, the stratosphere warms sharply in an event known as sudden stratospheric warming, in just a few days, miles above the Earth’s surface. The warming weakens the polar vortex, shifting its location somewhat south of the pole or, in some instances, ‘splitting’ the vortex up into ‘sister vortices’.

The split higher up in the atmosphere can give rise to both, sudden and delayed effects, much of which involves declining temperatures and extreme winter weather in the eastern US along with northern and western Europe.

A sudden stratospheric warming also leads to a warm Arctic not only in the stratosphere but also in the troposphere as well. A warmer Arctic, in turn, favours more severe winter weather in the Northern Hemisphere mid-latitudes including the eastern US.

But the polar vortex is not a recent phenomenon. It has been tormenting the Earth’s northern regions for well over four billion years.