. . WEATHER: A Deep Dive into the Polar Vortex . . A Deep Dive into the Polar Vortex By Rick Grow January 7 at 10:34 am Washington Posthttp://www.washingtonpost.com/blogs/capital-weather-gang/wp/ 2014/01/07/a-deep-dive-into-the-polar-vortex/?tid=pm_local_pop
. A shorter URL for the above link: . http://tinyurl.com/ko3kk8l . .As eerie as it sounds, there is no need to dramatize the polar vortex. It is not new. We have faced bitterly cold air before, and we will face it again.
.The polar vortex is really just a large air mass that is extremely cold (temperatures fall below -78C, or -108F, during the Northern Hemisphere winter). This concentrated area of cold is encircled by a fast-flowing river of air called the polar night jet. Basically, the jet with its swiftly moving air current traps the vortex over and near the poles, north and south.
.Though the vortex is present throughout the year, it really comes alive toward the winter. Temperatures cool off dramatically with the loss of sunlight in the polar region. The cooling temperatures force the vertical layer of air within the vortex to shrink because the colder air becomes, the more dense it gets. The increased density lowers the volume of air (density and volume have an inverse relationship), hence the shrinkage.
.On a weather map, meteorologists identify areas of low and high heights to identify the polar vortex. The low heights represent regions where the vertical layer of air at a certain elevation is compressed, while the high heights indicate regions where the layer of air is expanded. Think of it this way: an area of low heights signifies that the air here is quite dense and, hence, cold; an area of high heights tells you that the air here is quite light and, hence, warm.
.The polar vortex is most certainly an area of low heights. Meteorologists most commonly analyze it at the 500 mb pressure level, which is roughly 18,000 feet above the ground. At this level, it looks like a massive low pressure system with a characteristic counterclockwise circulation.
.There are times during the winter when this circulation goes off the rails. Waves continually move upward through the atmosphere in the Northern Hemisphere; sometimes, these waves crash into the polar vortex. If this wave-crashing activity is strong and persistent enough, the vortex will begin to weaken and parts of it literally chunks of brutally cold air will break off into one or all of the three big continents (Europe, Asia and North America).
.Below is a loop of the 500 mb heights over the last 30 days. Blue colors indicate areas of relatively low heights. At the beginning of the loop in early-mid December, the polar vortex is easily identifiable. Note how it had a home base between Canada and Greenland (close to Baffin Bay). In late December, the vortex began to split apart and, by the start of the new year, a large piece of it escaped to the south over Quebec. Bitterly cold air accompanied this piece of the vortex last Friday and Saturday, with snow-covered areas of the Northeast feeling the most extreme cold.
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