Part I and II recapped the temperatures and snowfall for last winter. Why did these temperatures and snowfall occur? What were the individual drivers of each period last winter? I am sure I will miss some features in this long post so let me know. We start in October with our first snowfall of the season.
Strong cold front with a ton of vorticity spun up over the Great Lakes. Temperatures at 1000 feet off the ground (850 mB level) dropped to between -4 and -6 the night of October 18th.
Vorticity |
850 mB temperatures |
500 mB height anomalies were extremely low and deep
500 mB height anomalies |
Cold temperatures were widespread across the central US and Ohio Valley
This resulted in light accumulations across the eastern 1/2 of northern Ohio
By November, the pattern became more variable. First 10 days of the month featured well above normal temperatures followed by a sharp cold spell then another milder stretch around Thanksgiving.
Snowfall forecast for northern Ohio
Wave height on Lake Erie
December temperatures were overall below normal with a quick rise by New Years Day.
The ridge in the Pacific shifted north of the Arctic Circle. Trough developed across the Great Lakes and then the COLD. Strong Greenland ridge developed.
Arctic Oscillation Phases |
North Atlantic Oscillation Phases |
MJO phase and magnitude in March |
In summary, the colder March pattern shift was the result of many factors? First since mid/late February, the temperatures in the upper atmosphere had been warming over the North pole. The sudden warming in the stratosphere over the pole translates to high pressure over the north pole at the surface with colder temperatures and often a weaker polar vortex. (
Great graphic below showing the warming in the upper atmosphere from November through March. As the polar vortex weakened, the displacement propagated down into the lower atmosphere first in late December. It rapidly strengthened in January. Then a late February warming with a downward propagation in March and again in late April
Polar Vortex Behavior from Nov to April (red indicates weakening--colder) |
These changes high in the atmosphere over the pole propagate to the lower levels and further south into the tropical regions. These changes intensified the MJO (Madden Julian Oscillation) as it transitions out of warmer phases (2-3-4 much of the winter) to colder phases (8-7-1). (see MJO images above) The jet stream responded with more variability off of eastern Asia east over the northern Pacific and into North America. This has resulted in high pressure developing near Alaska and low pressure undercutting north of Hawaii. Greenland high pressure which reinforced the undercutting storm track strengthening the jet stream and the trough as it moved east into the Ohio Valley along with colder air.
Overall March temperatures vs normal. Notice little relative warmth.
All of this occurring in a slowly decaying La Nina along the equatorial Pacific. Blue colors (cooler water)
If this late season pattern shift would have occurred 6 weeks earlier, our winter would have been MUCH different: COLD and more SNOW in January and February.
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