I put my shovel away for the season. It's not coming back out. As I said to a friend only the other night over my third beer, "Climate change has been a bust, eh?"
Remember the polar vortex of 2014? Remember hoping like mad that this was one of those once-in-a-century anomalies? The weather people on TV are remarkably silent on this, but it wasn't an anomaly. We're back where we were then, victimized by this loopy jet stream that's not going away.
According to Rutgers University climate scientist Jennifer Francis, the very thing that started all this weird weather, global warming, has caused the once-blazing white (reflective) surface of the North Pole to turn black and spongelike. So the polar region is absorbing sunlight, which itself accelerates melting and warming … but alas, not the sort of warming that Minnesotans get to enjoy.
Oh no, it won't get hot here until July. Then we will find ourselves sweltering in a tropical rain forest.
We already have that, you say? You ain't seen nothin' yet, Minnesota. I'll get to the moisture issue in a minute.
The old-school jet stream that delivered relatively consistent seasonal change was created by colliding hot and cold air. It had the same effect as a corset does on a person's midriff. As you age, the abdominal muscles weaken. Alas, the jet stream, too, is getting flabby. As the Arctic warms, the tension between cold and hot air masses is reduced. Francis compares the effect to that of a table tilting first one way and then the next before settling into a slope that pulls the heavier warm air north, which in turn pushes cold air south.
Not as far south as Oklahoma, though, where a heat wave is promoting wildfires as I write, thanks to the same forces bringing us blizzard-like conditions. Our 21st-century weather can be wildly counterintuitive. New York City will enjoy a humid 80-degree weekend, while in New York state's capital, Albany, temperatures are expected to drop to 32 degrees. This is owing to the jet stream's other exciting new feature — swirling eddies that spin off the main jet stream and wreak regional havoc.
Other factors influence the jet stream, most notably the fact that our planet spins like a top. There is also topography — mountain ranges and prairies and the like.