[QUOTE=xtisme]
I’ve heard this before but I’m not sure I get it. Wasn’t the average global temperature much higher in the past…say before the mass extinction of the ‘dinosaurs’ (at various times)? I seem to recall that during several of those periods there were huge inland sea’s in the US, and that much of the South West and the great plains were either under water or pretty lush habitat…much more so than today. And in the north there were vast tracks of very good habitat under what is basically snow today.
I don’t know what the sizes of deserts were then, but I know that, say, the Gobi was ALSO pretty lush habitat at one point when the world was much warmer…and as I said the south west in the US was pretty good habitat (when it wasn’t under water I suppose :)) in the past as well. IIRC, the Sahara and Northern Africa ALSO was pretty good habitat at one time…as well as Siberia.
My guess is that my mistake is that these places weren’t all good habitat at the same time (i.e. they were good at different times in the past)…and that this is just the tip of the ice berg of what I DON’T understand about all this climate changing stuff. Could you explain why it will be different this time than it was in some of these past (much warmer) climates?
-XT
[/QUOTE]
Hunting around for something related to a fact that surprised me in my college geology course, I found this page which explains some things pretty well.
Deserts are not randomly distributed. Current deserts across the world are centered at about 30 degrees latitude north and south of the equator. The reason for that is that global air circulation is currently in resonance in such a manner that hot air rises from the equator and cycles back downward at those latitudes. As it rises, it cools, and the moisture it contains (you will notice on the same map you looked at to verify the desert pattern that there ain’t a whole lot of land at the equator) precipitates out. When the air is cool enough to descend at 30 degrees, it is dry as a bone, and then gets warmed by the earth as it descends. Voila! Desert.
There are a lot of factors that go into making atmospheric circulation resonate the way it currently does, but as my linked page shows, 8,000 years ago it must have been circulating differently, because the Sahara was lush back then.
It’s a combination of temperature patterns, ocean currents, the specific location of major mountain ranges, etc. And since the Earth’s crust is just a bunch of big rocks bobbing around on top of the mantle, rocks which rise, fall, bend and tilt over time, and the continents are just the parts of the thicker areas of crust that happen to be sticking out above the waterline, the distribution of major landforms is much much different now than it was in the time of the dinosaurs. This affects ocean and air circulation both, and means that it was literally a different world back then. Our current world just happens to be made of some of the same rocks the old one used, and they tell the tale.