10 K/km (in the troposphere)
Are formed yes
Roughly 3 degrees per thousand feet
the water is using heat to undergo a phase change , the water's latent heat of vaporization is being pulled from your body
* Rising Unstable air * moisture * Air cools with an increasing altitude
A belt of dry hi pressure air
Latent heat is an important form of atmospheric energy. Latent heat is a property of water vapor in the atmosphere and when water vapor condenses it releases latent heat. Latent heat must be supplied to evaporate liquid water and this heat affects the behavior of the weather.
Rising air cools and compresses adiabatically.
Are formed yes
rising air expands then cools and condenses
it circulate through this way, from man to plant to man
First we need to know how cumulonimbus clouds in general form. Cumulonimbus clouds develop when the atmosphere is unstable. Generally, air temperature drops with increasing altitude, and warm air tents to rise through cold air. But, when air is made to rise it decompresses and cools. Under most conditions this air will soon become cooler than the surrounding air and sink back down. In this situation the atmosphere is said to be stable. If, however, the rising mass of air remains warmer than the surrounding air it will continue to rise on its own buoyancy and the atmosphere is said to be unstable. In the case of a cumulonimbus cloud this instability is provided by moisture. Water vapor holds a lot of energy in the form of latent heat. As a rising moist air mass cools the moisture in it condenses into clouds and rain, releasing its latent heat. The energy release dramatically slows the rate at which the rising air cools, so it remains warmer for longer. If there is enough heat and moisture, and the atmosphere is unstable enough the rising air mass will form a cumulonimbus cloud. Eventually the rising air mass will reach the same temperature as its surroundings and stop rising, forming the distinct flat top of a cumulonimbus. More latent heat and a colder upper atmosphere lead to taller cumulonimbus cloud. Since the height a cumulonimbus is an indicator of the degree of instability, the tallest thunderstorms are usually the strongest.
the magma cools on the surface and eventually u get land
Roughly 3 degrees per thousand feet
Condensation occurs on the windward side of a mountain. The rising air cools so the air becomes saturated and the water vapor condenses and causes it to rain.
I think you must mean the 'latent heat of fusion' experiment where a change of state in the cooling curve of a hot liquid like naptha or Octadecanol. the liquid cools as expected until the liquid starts to solidify. The temperature drop is arrested as the crystallisation process emits latent heat. Having solidified it then cools as expected.
the water is using heat to undergo a phase change , the water's latent heat of vaporization is being pulled from your body
* Rising Unstable air * moisture * Air cools with an increasing altitude