Over at the Hockey Schtick, Michael has an interesting new angle on determining planetary surface temperature from pressure and gravity – a subject covered extensively here at the Talkshop over the last three years. Here’s an extract. Of particular interest here is his new method of using the centre of mass of the atmosphere as a reference point. Head on over to read the full post.
Step 2: Determine the height at the center of mass of the atmosphere
We are determining the temperature gradient within the mass of the atmosphere and the equilibrium temperature is thus at the center of mass. The “effective radiating level” or ERL of planetary atmospheres is located at the approximate center of mass of the atmosphere where the temperature is equal to the equilibrium temperature with the Sun. The equilibrium temperature of Earth with the Sun is commonly assumed to be 255K…
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