I'm an inventor of mechanical engineering and civil engineering devices related to climate, but I'm also inquisitive about climate change theories. So, please let me try to nose around and poke a hole in something here.
> The heat flux has two elements, sensible heat flux ie warm dry air of
temp T and
> latent heat flux ( so called) which is the movement of water
vapour ( qv)
> which releases latent heat when condensation occurs.
Is purely vertical latent heat flux a major factor in regional greenhouse temperatures? Often the Amazon Basin at the equator hits a high of 30 degrees Celsius and the Sahara Desert well north of the equator hits a surface high of 50 degrees Celsius, Conventional wisdom says that the Amazon Basin has more cloud cover, but how does the Amazon shed so much of the solar heat that does reach its surface? Why doesn't the heat just build up in any rain forest as it does in any desert?
is the temperature discrepancy because purely vertical latent heat transfer is moving the heat straight up as high as 15 kilometers, into the stratosphere, where the newly relocated heat energy is now above 90% of all atmospheric greenhouse gases? At this great altitude, given a certain unit of time, does far more of the heat radiate farther off into space and so it becomes gone, rather than heat staying at ground level in the desert and radiating back down onto the ground? High in the stratosphere, the earth's insulating blanket is pretty thin, a threadbare and chilly insulating blanket if you might wish for a more human description for the insulative effect.
Vertical latent heat transfer is noteworthy because a mole of H20 molecules will mass 18 grams, 16 grams for the one oxygen atom and one gram each for the two hydrogen atoms. A mole of H2O-free air molecules averages 29 grams because air is roughly 80% N2 atoms and 20% O2 atoms. So, 24.5 liters of moist air will have less mass than 24.5 liters of dry air, and currents of moist air will rise in the atmosphere if temperatures are equal. That's how thunderstorms happen.
H2O is a greenhouse gas, but what if it's equally a heat-dumping transfer system on much of planet earth? This theory of latent heat transfer nfluences at least some of my climate-restoring mechanical inventions. It will also influence the science behind creating tiny sea salt particles and then wishing against hope that they will rise into the planet's stratosphere for you.
Yours in Hope,
Paul Klinkman