I had noted the temperature was actually getting warmer as I did the weekly hike up Spencer Butte with the Club. No, it wasn’t just that I was working hard, but it was cold at the bottom, and it wasn’t nearly as cold a thousand feet higher. We hike up to the top from the city, 3.2 miles gaining 1400 feet of elevation. Slower hikers leave earlier; sometimes, I decide to leave early if I am rehabbing part of me, and other times I leave early so I can hike alone. Often, I have a line of people behind my, liking my pace, but making me feel like the Pied Piper. I don’t like such a situation, for I tend to walk faster, when I am already at cruising mode, and I get tired sooner. Once I stopped suddenly on a hike to take a picture and got run into by the guy behind me. I learned that backpacking through Alaska willows and other brush. Don’t crowd the person in front. They may have to suddenly stop, and they have sharp hiking poles. That can slip. Anyway, the summit of the Butte is finally reached after a series of rock steps, about 130 altogether, not counting the occasional smaller ones, and I looked down on a foggy, cold valley from the land of blue skies and sunshine.
Off to my northeast, the mill in Springfield had a plume of smoke rising in the sky then flattening out and spreading along an invisible barrier like a river. I could see about fifteen miles of the smoke river, coming first towards me then moving away to the northwest.
Wow, I thought, a classic inversion. Warm air normally rises, and it normally keeps rising as the atmosphere usually gets colder with height. Valleys during winter collect heavier cold air as it sinks, and set up an inversion, where warm air rises through the cold air until it reaches the warm air above—not below—and stops rising. I first noted it in southeastern Arizona, back when I was commuting from Tucson to Las Cruces for graduate school. Once, on a bike, I went through a thick fog bank going up to Mt. Lemmon, breaking out at about 4000 feet into bright sunshine and a dew point temperature, where water will condense into clouds, 30 degrees fewer than just a few hundred feet below. Those who turned around in the fog missed a sunny day, which was about five minutes’ ride further up the mountain.
My wife and I hiked through an inversion in the Grand Canyon in February 1989, when the whole canyon was full of clouds and bright sunshine up at Yaki Point. We hiked down the South Kaibab, entered clouds, then broke out below into overcast conditions. It was remarkable.


Back on Spencer Butte, I waited for others to come up and googled the University of Wyoming’s weather sounding page. The closest weather balloon released was from Salem, about an hour north, and indeed showed a change in temperature of 0 C (32 F) at ground level and 10 C (50 F) at 1500 m or 5000 feet. Classic inversion, I noted, staring at the river. I told a few people about what we were seeing, but nobody seemed interested.
Back then, I was still posting on Facebook, and I later posted the picture and the weather sounding as a textbook example of an inversion. Here is another example, with a link to the actual weather at that hour.

Facebook is not the land of people’s liking textbook examples explaining physical phenomena. I got exactly one comment, a nerd icon, which I didn’t even know such existed. It wasn’t the reason I left the platform, but it was one of the accelerants. I haven’t missed the sniping, arguing, or ignorance since I left it. Nope. I try to walk in beauty the way the Navajo Prayer says.
A decade prior, I had been hiking on the South Rim Trail in Big Bend National Park up to the overlook over the Chihuahua Desert. I was alone, and as I hiked on the rim, I saw an area that looked like smoke, then steam, a quarter mile ahead of me. I arrived at the area and saw water vapor condensing to form a cloud, right in front of me. I was on top of a cliff, and the humid southerly wind from deep down in Mexico, had slammed against the cliff, forcing the air upward, where it cooled, since in summer the inversions are usually shallow and break. Cool air condensed once it reached the dew point, which is higher in summer, and a cloud formed right in front of me. This is orographic lift, and I was absolutely enthralled at the example I was seeing.

I was naive enough to think that The Weather Channel might be interested in a picture, so I sent one to them. I didn’t hear anything, not surprisingly, but I was disappointed.
I get great pleasure out of seeing things in nature that are not only beautiful but enhanced because I’ve been fortunate enough to be brought up curious about the world. A total solar eclipse is beautiful not only because of the color of the chromosphere or the thin strands of the corona, but because it is the resonance of three separate lunar cycles—the synodic, the anomalistic, and the draconic—which every 18 years and 10 1/3 days are almost exactly the same, so that the eclipses repeat every 18 years and change plus 1/3 of the way west around the world. I find that fact fascinating.
On the Libyan cruise to the 2006 eclipse, an editor of Astronomy magazine discussed eclipses to the audience. He didn’t mention the cycles, and I suggested afterward that perhaps people might like to know that. “Nah,” he saiid, “that’s too nerdy.”
That came from an astronomer.

Normally, I don’t write about this sort of stuff, because most people aren’t interested. I would simply say that
In beauty I walk…
In beauty all day long may I walk.
Through the returning seasons, may I walk.
On the trail marked with pollen may I walk.
With dew about my feet, may I walk.
With beauty before me may I walk.
With beauty behind me may I walk.
With beauty below me may I walk.
With beauty above me may I walk.
With beauty all around me may I walk.
In old age wandering on a trail of beauty, lively, may I walk.
In old age wandering on a trail of beauty, living again, may I walk.
My words will be beautiful…
