Comments by "" (@1965ace) on "Sabine Hossenfelder" channel.

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  28. ​ @chrisa.4937  Let's really discuss the basic physics of daytime heat energy transfer. So I'll stipulate that IR directly from the sun is mitigated by GHGs. In addition let's agree earth is radiating surface heat into space both day and night. So now we can concentrate on the mechanism of heat transfer to and from the lower atmosphere. As far as average global temperature is concerned that is completely dependent on the rate of energy transfer in each cycle (there is no static retention of heat only rate of gain and rate of loss). To understand it on the smallest level will disabuse one from making cause and effect assumptions on a bigger scale. So our source is higher energy radiation (light) that hits earth's surface. This is then (excluding photosynthesis and other chemical reactions) is converted to increasing kinetic molecular activity (temperature) on the surface. Warming surface temperatures are losing heat to conduction, subsurface earth and water, convection (kinetic activity in the atmosphere next to the surface and progressing vertically) and radiation (long wave infrared light). Here is a model I use to give one a subjective understanding. Picture a camp fire on a cold night. Standing not too close we can feel the radiation warm our skin absent most the convection that will increase by getting closer. Now at the same distance feel the heat directly above the fire. The reason it feels much hotter is the convective transfer is rising. The higher we go the more of that convective heat is absorbed by cooler surrounding air. If you don't have any major issues at this point we can continue to the next step.
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  29.  @chrisa.4937  The reason for understanding each process is to have a complete cause and effect ground we can agree on. So a warming surface is radiating and convecting as our starting point here. To understand GHG's absorption and emission of IR will give us another part of the picture. Absorbtion and emission are equal for any given substance. So let's say a CO2 molecule is at an energy state lower than the surrounding radiation, this puts in a state of Absorption to receive energy equal to the surrounding radiation. That will increase it's temperature (kinetic molecular energy). It is now in a state of equilibrium with the surrounding level of radiation, and doesn't absorb more radiation. Since temperature is the average molecular kinetic energy of a system and CO2 cannot absorb more radiation than source emits, to continue warming the atmosphere the energy has to flow to a lower state such as a nitrogen or oxygen molecule and that happens during a convection event when the CO2 molecule bumps into a cooler nitrogen molecule. The nitrogen warms and the CO2 cools to a close state of temperature equilibrium (increasing entropy). Now the CO2 molecule is again at a lower energy state and may be able to absorb radiation again. (I said may because light can only be absorbed and emitted in specific levels ). So to increase atmospheric temperature the bulk of kinetic molecular energy has to increase, aka nitrogen and oxygen warming from surface convection and radiation that is absorbed and convected to those gases. I want to go on but I really want to be on the same page for the physics of what is happening. Remember Einstein once penned " to (really) know a thing is to be able to explain it in simple terms but no simpler".
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