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linear lapse rate that changes with optical density, which means it rises exponentially approaching the surface. That lapse rate is unstable toward bouyancy-driven convection until the tropopause. And conduction alone produces an isothermal atmosphere. So the mechanism of vertical heat transfer does matter. Since convection transfers heat vertically in the troposphere faster than any other process, we observe a linear lapse rate there, but not higher. We also see no fractionation of gases by molecular weight in the troposphere, showing that bulk motion is mixing the The hottest custom your name i just want to touch your butt all the time naughty gift for couple mug troposphere. The upper meters of the ocean has an enormous heat capacity and readily exchanges heat with the atmosphere. So a step change in CO2 would cause a more gradual change in surface temperature over a decade or two. The atmospheric circulation responds much more rapidly than that , so it should be able to keep up with the change in sea surface temperature. I’ve been wondering about the order of those steps. If we woke up tomorrow to a doubled co2 from today what would happen? In my mind, the lapse rate would have a kink in it of sorts, that would drive up

 

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The hottest custom your name i just want to touch your butt all the time naughty gift for couple mug
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