Ziggurat
Penultimate Amazing
- Joined
- Jun 19, 2003
- Messages
- 61,735
Surely, you aren't echoing Mr Goddard and trying to bring WUWT woo pseudoscience into a legitimate discussion of Venus,...are you?
"adiabatic" - occurring without loss or gain of heat
Highly unlikely with respect to Venus and the issue of its atmospheric and surface heat content. There are some adiabatic processes playing important roles in the atmospheric physics of Venus, but by definition, adiabatic processes are energy neutral
They are heat neutral. They are NOT energy neutral. There's a major difference.
and don't seem particularly relevent to issues of Venus' surface/atmosphere heat
It's damned relevant. Hell, it's very relevant to earth's surface temperature too. That's why Death Valley is so damned hot: it's below sea level.
nor any proposed nullification of the CO2 greenhouse effect.
This isn't about a nullification of greenhouse effects. It's about the relative sizes of effects. And atmospheric thickness effects will dominate over greenhouse effects when you want to discuss the difference in surface temperature between, say, Earth and Venus.
I'd recommend "The Recent Evolution of Climate on Venus" Bullock & Grinspoon as a good reference on Venus's heat.
Composition will be VERY important to the upper atmosphere temperature. But lower down, it becomes much less important. Look at figure 2 of your paper. Below about 40 km, notice how the temp vs. altitude graph becomes pretty much a flat line, fairly close to that 10 C/km adiabatic lapse rate I cited earlier. That's not radiative heat transfer. Yes, adiabatic compression and expansion aren't the ONLY factors at play, but they are the dominant component at lower altitudes. So whatever you want to do to the upper atmosphere, you'll still have that slope at lower altitudes, and you'll still end up with a surface temperature MUCH hotter than Earth's, regardless of what you do to the composition. That paper doesn't actually claim otherwise. In fact, let's see what they say about adiabatic processes:
"Convection was treated by taking the radiative equilibrium temperature profile and adjusting the lapse rate to be adiabatic wherever the radiative
equilibrium lapse rate exceeded the adiabat (McKay et al. 1989)."
Hmm.... seems they thought it was important after all.
