Transcript
A (0:00)
Today on Inevitable. Our guest is Joel Gratz, founding meteorologist and CEO of Open Snow. If you skied this winter, or tried to, you probably felt this season in your bones. It was one of the worst Western snowpack years on record in the U.S. joel is the person more skiers and snowboarders turn to than anyone else for snow forecasting, and he has a more nuanced take on what actually caused this season than you might expect. We get into that and then zoom out to what snowpack means for Western water supply, what climate change is and isn't doing to mountain snow, and what a well adapted ski industry might actually look like. Good one to close out the season with. From McJ, I'm Cody Sims and this is inevitable. Climate change is inevitable. It's already here, but so are the solutions shaping our future. Join us every week to learn from experts and entrepreneurs about the transition of energy and industry. Joel, welcome to the show.
B (1:17)
Thanks for having me. It's good to be here.
A (1:19)
We were just jamming a little bit on this right before we hit the old record button, but it seems like we came out of, from what I've understood, I didn't get to go skiing this year, unfortunately, but it sounds like we came out of one of the worst western snowpack seasons on record. And I found some interviews and quotes where you basically said, hey, this isn't a climate change story. And so what is it? Maybe I'd love to hear a little nuance there about how you think about that.
B (1:44)
Yeah, for sure. So first thing, the records go back various amounts of time, 40 years, 70 years, sometimes a hundred years. So this was very bad for snowfall, less so for precipitation at least we'll get to that. But for snowfall, for sure, this was very bad for the past many decades. If you look back over hundreds or even a thousand years, you will likely find in long term records kind of buried in sediments or tree rings that the west is prone to busts and booms. So I doubt that this is out of the bounds of what we have seen before, but it was bad. You know, just to throw that out there from a snow perspective, from a precipitation perspective, interestingly, it wasn't as bad, meaning that they were still a decent amount of precipitation. But the challenge this year was the warmth. So it is mostly not a climate change story, but also somewhat of a climate change story. So let me dig into that. The mostly not a climate change story is that we just had bad luck. It was below average precipitation and very, very warm and the atmosphere is chaotic and sometimes you get the bad end of the chaos and it's not good. And look at what happened on the east coast, and we're Talking about the 2025, 2026 winter season here in North America. The east coast and New England had a wonderful winter. So oftentimes the atmosphere balances out and one place gets a lot of snow, another place doesn't. So partially this is just a bad luck story with a lot of variability in the atmosphere. The more nuanced version of that that does implicate climate change is that on average, temperatures are warming. Warming temperatures will mean generally less snow on the shoulder seasons of fall and spring, when the snow is often competing with rain. Is it cold enough to get snow versus rain? Well, one or two degrees in either direction can push that in a way that us skiers don't like, also at lower elevations. So at elevations that have always been close to the rain snow line. Now I'm in Colorado. Rarely does rain happen on most of the ski areas here. But you're in California, it is a very normal thing for the skiers to be dealing with a rain snow line and along the East Coast. So from a climate perspective, even a slight trend toward warming temperatures will generally push the odds maybe a little bit more towards rain than snow when we have these edge cases. So to wrap up, mostly this is a season of bad luck when it comes to snowfall. But the background warming of climate change likely has some role in just the warmth. Not the major role of the warmth, but some role in the warmth.
