rollin wrote:April Fools?
.An earlier article in Chemical Innovation (1) showed that if you believe that biology’s mouse-to-elephant curve also applies to the flying creatures of the past, and if you also trust aerodynamic theory (which applies equally to flying insects, birds, and airplanes), then the giant flying creatures of the dinosaur age could only fly if the atmospheric pressure was much higher than it is now: at least 3.7–5.0 bar.
If this is so, it raises several interesting questions. For example, how did the atmosphere get to that pressure 100–65 million years ago (Mya)? What was the pressure before that? And how did it drop down to today’s 1 bar? Although we have no definite answers to these questions, let us put forth reasonable possible explanations.
Figure 1. Three possible alternatives for the atmospheric pressure early in Earth’s lifetime, given that it was at ~5 bar, ~100 Mya. What was the air pressure for the 97% of Earth’s life before the age of dinosaurs? We have three possible alternatives, as shown in Figure 1.
The pressure could have been at 1 bar throughout Earth’s earlier life, risen to 4–5 bar ~100 Mya (just at the time when the giant fliers needed it), and then returned to 1 bar (curve A).
The pressure could have been ~4–5 bar from Earth’s beginning, 4600 Mya; and ~65 Mya, it could have begun to come down to today’s 1 bar (curve B).
The atmosphere could have started at higher pressure and then decreased continuously through Earth’s life to ~4–5 bar ~100 Mya and down to 1 bar today (curve C).
The third alternative seems to be the most reasonable, so let us pursue it. We will also look into the composition of Earth’s atmosphere, but we will first discuss Earth’s surface and see how it affects the atmosphere.
rollin wrote:Earth's atmosphere at 90 Bar, mostly CO2, would have been far too hot for the water vapor to condense and thus start the removal of the CO2 as the "paper" states.
Very high atmospheric pressures on the 3 to 5 bar level (denser atmosphere) would have changed the size of lungs and gills dramatically, making them much smaller than present. Plants would needed far less stomata than presently needed. I have never come across any evidence of that, it would be a hugely significant difference. Any evidence of that?
rollin wrote:This is amazing -from the "Earth's atmosphere before the age of dinosaurs"
"Figure 5 verifies the earlier statement that the present oceans are relatively young because they contain limestone not older than 200 million years. On the other hand, the continental landmasses are much older because, 100–65 Mya, the oceans and the atmosphere shared the free CO2 equally. Consequently, the pressure of CO2 in the atmosphere was ~8–10 bar in the age of the flying creatures (Figure 6)."
Do they know what they are saying? The earth's atmosphere had 20,000 times the amount of CO2 in it during the coal age!! Absolutely amazing that proteins could exist at those temperatures. This is a whole new kind of science!
Actually an old one - it's called Snake Oil.
Alfred Tennyson wrote:We are not now that strength which in old days
Moved earth and heaven, that which we are, we are;
One equal temper of heroic hearts,
Made weak by time and fate, but strong in will
To strive, to seek, to find, and not to yield.
rollin wrote:Here is an interesting article on life and the evolution of Earth's atmosphere
http://www.amnh.org/learn/pd/earth/pdf/ ... sphere.pdf
Alfred Tennyson wrote:We are not now that strength which in old days
Moved earth and heaven, that which we are, we are;
One equal temper of heroic hearts,
Made weak by time and fate, but strong in will
To strive, to seek, to find, and not to yield.
sparky wrote:.
The pressure does not create the temperature
by itself it is just neutral , temperature must be gained from something , then re-emitted
As a though experiment think of a well insulated maze ,
mice come in , then come out ,
the time spend inside depend on the " density "of the maze
the more time spend , the more mice inside the more effort to get out
would increase the temperature inside
I know it's a bit silly , but gas density of the atmospheric maze does not heat up anything by itself
Total solar irradiance , internal planetary heat and the odd meteorite crash are the input
radiative cooling is the output
Return to Environment, Weather & Climate
Users browsing this forum: No registered users and 25 guests