a fan of *MORE* discourse: • ignorance that feels like knowledge, and
Maybe you know the answer to my questions.
1. If the Earth surface warms by 1C, how much does the rate of evaporative-transpirational transfer of energy from surface to upper troposphere change?
2. Does that change increase or decrease the cloud cover? — In what regions?
3. Does it increase or decrease rainfall? — in what regions?
4. In the places and times that generally produce evaporation (e.g. early summer days in the American Midwest), what are the net effects of an increase of 4W/m^2 downwelling LWIR? (evaporation, cloud cover, rainfall.)
My ignorance of these topics feels much like ignorance. If you know who has the information and where it has been published, please share it. As you probably know, Romps et al recently derived the result that a 1C increase in the surface temperature would produce a 12% increase in the lightning rate; apparently with no increase in the rate of evaporative-transpirational energy transfer that produces the clouds, rain, and lightning in the first place. Perhaps you can fill in the gap here between the surface warming and the lightning bolt increase.