Showing posts with label Low Pressure. Show all posts
Showing posts with label Low Pressure. Show all posts

Tuesday, October 26, 2010

BOMBOGENESIS!

Bombogenesis is defined as rapid or extreme cyclogenesis of a mid-latitude cyclone that drops in surface barometric pressure by 24 or more millibars in a 24-hour period.

A record-breaking weather event is unfolding across the upper Midwest of the United States as I type this. Surface pressures are rapidly falling and the winds are kicking up big time. Why is it happening and how significant is it?

In a case of classic bombogenesis, this storm's surface pressure has been steadily falling and is expected to fall by at least 24 millibars in 24 hours. Bombogensis is not something you often see in this part of the country, but for those in the tropics (hurricanes) and the northeast (nor'easters), it's not that unfamiliar of a term.


Current surface maps as of 10:00 a.m. ET, October 26, 2010

So how could this storm stack up with other notables in the region? In a tale of "GREAT" 'Great Lakes' Cyclones,' the developing storm could go down as the second strongest cyclone
(in terms of pressure) to move through the region since record keeping began. Check it out...

1. The Great Ohio Blizzard - January 26, 1978 (958mb/28.05 inches)
UPDATE 10:30 p.m. ET, October 26, 2010: Now the #2 storm.

2.
CURRENT STORM - October 26-27, 2010 (959mb/28.35 inches)
UPDATE 10:30 p.m. ET, October 26, 2010: The current storm has become the #1 storm at 955mb/28.20 inches.

3. Armistice Day Storm - November 11, 1940 (967mb/28.55 inches) and Anniversary Storm - November 10, 1988 (967mb/28.55 inches)

4. Cyclone of 1913 - November 7-9, 1913 (968mb/28.60 inches)

5. Edmund Fitzgerald Storm - November 10, 1975 (980mb/28.95 inches)

Speaking of the
Edmund Fitzgerald Storm, check out his tribute...



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Friday, January 29, 2010

Atmospheric Inversion: Utah's Winter Woe

What is an atmospheric inversion? And why every winter is it the talk of the town (city) in Salt Lake?

Meteorologically speaking, an inversion is a deviation from the normal change of an atmospheric property with altitude. Big deal right? Here's why...

When a warm air mass moves over another cold, dense, air mass -- as it often does during winter in northern Utah's Salt Lake Valley, that colder air mass settles into the land-locked valley, becomes heavy; and because of its weight and lack of wind movement at lower elevations, it cannot move. The end result is a visibly stagnant air mass in the form of low clouds, fog and/or haze.

So again, why is this a big deal? An inversion can lead to extremely dangerous pollution such as smog being trapped close to the ground, with possible adverse effects on health. This is why, believe it or not, Utah, has some of the worst air quality in the United States.

How does an inversion disappear? Typically an inversion only occurs when high pressure is dominating the troposphere (the lower region of the earth's atmosphere). During high pressure air sinks and becomes trapped. But when a low pressure system is overhead air rises, therefore lifting the inversion from the valley and disintegrating its associated pollutants from the earth's surface.

So what's the catch? If you like fair, sunny weather, deal with the inversion. If you don't want to deal with the inversion, you'll have to deal with it being stormy.

For those followers who needed a better understanding of what the inversion was, I hope The Northeast Quadrant was able to help!