Since the middle of March, we've been watching the potential for some pretty serious cold for early April around Opening Day at Progressive Field. There's been a lot of warming in the stratosphere over the north pole (warm colors below) which usually takes a couple of weeks under ideal circumstances to make its way down into the troposphere where weather directly impacts us. (Often times the stratosphere warming doesn't propagate down into the troposphere so the upper atmospheric warming remains, what we call, decoupled from the lower atmosphere. In those cases, little impact in the form of cold occurs.)
Warming at the top of the atmosphere creating cold at the surface seems counterintuitive but that warming and the stratosphere creates high pressure at the surface in the high latitudes. Here is a primer from NOAA. There are many ingredients that have to be present for this to occur. Some originate in the tropics which make their way to the pole.
Where that change propagates south is typically where the cold sets up. In many instances, the long-range computer models have a difficult time ascertaining this.
Here is European Model each day from March 26 through April 1 showing temperatures for Tuesday afternoon April 8th (Opening Day in Cleveland). Notice it didn't pick up on the cold over the Great Lakes/Ohio Valley until March 29. Each day the cold became stronger and more pervasive across the northern half of the country.
- There have been only seven games where we had game time temperatures in the 30s:
- The 2016 home opener was the coldest at 34°.
- 1899 opening day at League Park was the warmest. Game time temperature 84°.
- The most precipitation ever on opening day was 1981, April 11th at the old stadium. We had 1.44" of rain.