Perhaps useful in more depth than I see, but Willis has simply provided insight into how our uneven planet and all its fluids try to even out and dissipate the input energy from the sun. Nothing new, just a very astute observation of how it actually works out. The nonfluid parts are quite uneven, so the fluid flows and energy dissipation are also uneven. It shows in broad strokes why it is warmer and colder in various regions.
Good. Simple. Broadening understanding.
Guest Post by Willis Eschenbach
I got to thinking about the idea of a temperature field. By that I mean nothing more than an estimation of theoretical temperatures given some variables like say latitude and elevation. We all know that as we go poleward it gets colder, and the same is true when we go upwards into the mountains. So we can make a formula that can estimate the temperature at any spot on the Earth if we know its latitude and elevation. It’s an excellent estimation, with an R^2 of 0.94.
In the CERES satellite data, the relationship works out like this. Start at minus thirty-one degrees. Add sixty times the cosine of the latitude. Then subtract six degrees for every thousand metres of elevation. That gives you the estimated temperature for any given location. I note that the decrease in temperature at higher altitudes, about six degrees C…
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