Not exact matches
Condensation is a
phase transition of matter that occurs when water
vapor contained in hot, humid air comes in contact
with a cold surface.
The height redistribution in the atmosphere of condensation nuclei
with a change of the electric field of the atmosphere is accompanied by a change in total latent heat (
phase transition of water
vapor), by changes in radiation balance, and by subsequent changes of the thermobaric field of troposphere.
when you can design a model that can even predict a temperature profile of: a 4 degrees of freedom, rotating sphere, that is warmed by the output of a non-linear external heat source, and that is covered in a thermodynamic fluid that is constantly in motion
with non-linear chaotic Beyesian characteristics — and then throw in variability due to non-linearity behavior of an element that can cause both positive and negative feed - backs due to the existence of it's three
phases; liquid,
vapor and solid....
The gas -
phase reaction of methane sulfonic acid
with the hydroxyl radical without and
with water
vapor
I would believe a sensitivity to water
vapor should precede a sensitivity to CO2 doubling, CO2 is well mixed and easy, water
with its three
phases impacting both the surface and the atmosphere, not so much.
With decreasing temperature the equilibrium shifts to favor the liquid phase (with the caveat that the process can be very slow due to the empirically observed tendency of vapor molecules to bounce off droplets when intuition would suggest they would stick at first h
With decreasing temperature the equilibrium shifts to favor the liquid
phase (
with the caveat that the process can be very slow due to the empirically observed tendency of vapor molecules to bounce off droplets when intuition would suggest they would stick at first h
with the caveat that the process can be very slow due to the empirically observed tendency of
vapor molecules to bounce off droplets when intuition would suggest they would stick at first hit).
In the
vapor phase, water moves quickly through the atmosphere and redistributes energy associated
with its evaporation and recondensation.
However, as the water
vapor rises the lapse rate means that the volume of air cools and eventually the water
vapor condenses into water droplets and then into ice latent heat is given off to the surrounding air at each of these
phase changes,
with two effects.
The SGM doesn't have clouds and even if you put in an absorber
with a different scale height like water
vapor, it's never saturated, so there are no
phase changes above the surface.
With regard to suricat's ideas: When someone conflates the ideas of liquid / vapor phase transition with an El - Niño / La - Niña phase transition, and tries to bring in the Clausius - Clapeyron equation, I have to assume they are arguing by free - associat
With regard to suricat's ideas: When someone conflates the ideas of liquid /
vapor phase transition
with an El - Niño / La - Niña phase transition, and tries to bring in the Clausius - Clapeyron equation, I have to assume they are arguing by free - associat
with an El - Niño / La - Niña
phase transition, and tries to bring in the Clausius - Clapeyron equation, I have to assume they are arguing by free - association.
We propose a different source of potential energy associated
with water
vapor removal from the gas
phase: after the Mayan forests were destroyed, evaporation and condensation ceased to occur over the Yucatan peninsula (irrespective of how its albedo changed).