Atarimaster wrote: ↑Wed Aug 23, 2023 5:41 amHmmm.
I’ve seen Gall-Peters a couple of times, even outside of cartography discussions (probably no other cylindrical equal-area projections). But I don’t remember to have seen equirectangular maps in actual use (i.e. other than being a resource for map makers).
Maybe I
have seen some of them, especially on websites, but I don’t remember it.
I guess this highlights the need for actual studies rather than "I think I've seen this somewhere".
I know that one website that I actually use from time to time,
Great Circle Mapper (great for measuring distances between places and seeing what the paths look like), offers a choice of three projections: plate carree, orthographic (polar or oblique), or azimuthal equidistant (always oblique). Notably, its implementation of the equirectangular projection is rather poor, as even when mapping a small region, it's
always plate carree, instead of shifting the standard parallel into the relevant region. (Usually I use it with whole-world maps or regions large enough that it doesn't matter.)
On Wikipedia, the plate carree is used for the
world-by-meridian-or-parallel navigator, although here there's an actual strong reason to favor it over all other projections, rather than just using it as a compromise projection.
That's just what I can think of on short notice.
But you're probably right that Gall-Peters gets used more often than I gave it credit for, too. I figured that since its supporters mostly advocate it as an alternative to the Mercator projection, it wouldn't really appeal to people unless they were previously either using the Mercator projection, or didn't know any map projections at all. But then I guess such people do exist.
PeteD wrote: ↑Fri Aug 25, 2023 2:00 amWell, for "thing-per-area metrics", equal-area projections
should be used but aren't always,
There will always be idiots.
PeteD wrote: ↑Fri Aug 25, 2023 2:00 amIf the data shown isn't a "thing-per-area metric", then I don't see any particular reason to use an equal-area projection.
Well, it would still be helpful in showing how relatively common the high/low ends of the metric you're measuring are. Like, temperature isn't a thing-per-area metric (in the sense that a 200-square-kilometer area isn't twice as hot as a 100-square-kilometer area, although you might argue it does have twice as much heat energy...), but it can still be useful to know whether it's better to think of Earth as mostly warm with some cold spots, or mostly cold with some warm spots. (I would expect mostly warm with some cold spots, since 50% of Earth's surface is within 30° of the equator, although comparatively less of the
land is.)
Yes, it isn't
as important as when measuring thing-per-area metrics, but it's still valuable.
Of course, then you get to thing-per-capita metrics, where it might be useful to use a cartogram instead of a normal map projection...
PeteD wrote: ↑Fri Aug 25, 2023 2:00 amMilo wrote: ↑Wed Aug 23, 2023 4:17 amI've seen at least one case of an article using Mollweide, apparently as a scientific-community-accepted "default" map projection, in the one context that I really
wouldn't recommend its use for: a climate simulation of weather on a tidally-locked planet, where, of course, the effect of latitude relative to the equator is far less dominant than on normal planets!
What would you have used? A two-hemisphere projection?
Probably. Either that, or just a single azimuthal projection centered on the substellar point, depending on whether I prioritized reducing distortion or keeping the map uninterrupted.
(Note that Mollweide can technically be used to make a two-hemisphere projection too - they'll even look circular! - but that obviously isn't what we're talking about here.)