The overall pattern this spring has lacked substantial warm periods. Yes we've reach 80 degrees a few times earlier in May but nothing since. Add the high frequency of rainfall and this spring has been anything but pleasant. It's not only across northern Ohio but a large portion of the Great Lakes, Ohio Valley and central US.
Below are the temperatures compared to normal over different time periods since early April. Shades of blue represent below normal temperatures. Notice that most of the extremely "cool" air occurred in the last 2 weeks of May.
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| May 23 to May 30 |
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| May 15 to May 30 |
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| May 1 to May 30 |
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| April 1 to May 30 |
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| May 23 to May 30 |
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| May 15 to May 30 |
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| May 1 to May 30 |
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| April 1 to May 30 |
Interestingly, the Ohio Valley has had well above normal rainfall from Ohio, western PA south along the Ohio River including the entire deep south. Yet northern Indiana, Illinois and all of Iowa is running 2-5" below normal since early April.
Here is a close up look at Ohio's rainfall since early May:Why has this spring featured above normal rainfall and a high number of days with below normal temperatures? The answer is multi-faceted. First, the weak La Nina continues to weaken in the tropical Pacific. Second, the upper atmosphere over the North Pole went through a warming in mid March. (stratospheric warming). This resulted in the Polar Jet stream to buckle south resulting in periods of unsettled weather across the middle of the US and southern Canada this spring. It's been a slow developing process over the last 2 months. (If this "warming" would have occurred in January, the chances would have been much higher that this winter would have featured more extreme cold!)
The stratospheric warming is identifiable by looking at the high pressure over the North Pole. Notice that it descends down into the middle of the atmosphere. It tool a long time to "drip" deeper into the atmosphere after the initial warming in mid March. (graphics below courtesy Judah Cohen)
The trickle-down continued well into May.
The rise was accompanied by a reversal in the upper level winds. The red line which dropped below the blue dashed line shows this perfectly. This reversal weakens the polar vortex which allows more frequent periods of "cooler" air and an active storm track.
The upper level pattern in April shows the storm track across northern Canada, a ridge of high pressure across the eastern US/New England and the low developing in the SW US.























