Jump to content
Thunder?
Local
Radar
Hot?

Koppite

Members
  • Posts

    911
  • Joined

  • Last visited

Posts posted by Koppite

  1. The polar vortex is a persistent large-scale anti clockwise cyclonic circulation pattern in the middle and upper troposphere and the stratosphere, centered generally in the polar regions of each hemisphere. In the Arctic, the vortex is asymmetric and typically features a trough (an elongated area of low pressure) over eastern North America and over NE Siberia. The polar vortex is not a surface pattern. It tends to be well expressed at upper levels of the atmosphere (that is, above about five kilometers). When the polar vortex is strong, deep purples can be seen on the 500hPa charts as shown below:

    When these deep purples are situated over Greenland and Iceland then lower pressure dominates in the upper atmosphere which has a knock on effect to the lower levels. This tends to drive Atlantic based weather to these shores, giving us mild, wet weather. The stronger the polar vortex over the Arctic the Arctic Oscillation (known as the AO) will be more positive. When the AO is negative the polar vortex tends to be weaker and disrupted with areas of upper high pressure forming. These can 'block' the normal path of westerly surface low pressure systems and are known as blocking highs, and in the right position can lead to colder polar air heading southwards towards us.

    Thanks very much for that Chionomaniac, what is the AO at the moment positive or negative? I presume the blocking high you mentioned is the elusive Greenland high that most people on here wish for.

×
×
  • Create New...