When the relative humidity reaches 100 %, the water vapor
condenses into liquid water droplets and the clouds begin to form.
Exactly the same sequence of events, MUST happen, before water vapor can
condense into liquid water; but this time the latent heat that must FIRST be removed, is about 590 calories per gram.
Not exact matches
In simple terms, distillation involves evaporating the
water, and then
condensing it back
into a
liquid.
Bouillon comes from the French word «bouillir» which means «to boil» and refers to how chicken bouillon is prepared, since a combination of ingredients are simmered in
water and spices, until the
liquid condenses into a tasty broth that is full of flavor.
The temperature difference, as well as the high humidity inside the chamber, causes the vapor to
condense as
liquid water, which drips
into a collector.
Then colder
water is pumped from 800 to 1,000 meters below the ocean surface to
condense the steam back
into liquid form.
For any given temperature, it tells you how high you can make the partial pressure of
water vapor before the vapor starts to
condense into liquid or ice.
It originates in clouds when temperatures are below the freezing point (0 degrees Celsius, or 32 degrees Fahrenheit), when
water vapor in the atmosphere
condenses directly
into ice without going through the
liquid stage.
The main difference between H2O and CO2 (apart from the numerical differences of their specific physical properites such as degree of freedom, thermal capacity, physical mass, etc) in terms of their effects on the atmosphere is that
water is capable of
condensing into liquid to form clouds and readily and rapidly moves between surface and atmosphere, daily, seasonally, annually and on even greater time scales, but CO2 does not liquify in the biosphere and transfers over mostly long time periods between surface (primarily oceans, seas, etc) and the atmosphere.
Carbon dioxide is fully part of that
water cycle where
water heated by the thermal infrared direct from the Sun evaporates and anyway lighter than air rises in air and takes away heat from the surface — all pure clean rain is carbonic acid, the
water vapour spontaneously joining with carbon dioxide in the atmosphere releases its heat in the colder heights and
condenses out back
into liquid water and ice, cooling the Earth from the 67 °C it would be without the
water cycle.
What do you think happens to the energy that is released when
water vapour
condenses back
into liquid water?
By harvesting
water vapor from the air and
condensing it
into liquid, atmospheric
water generators can essentially pull
water from the air, and these devices hold a lot of promise for providing an independent source of drinking
water.
Do the models correctly account for the latent heat of evaporation of
water being carried up thousands of feet before releasing that heat energy well above the bulk of our atmosphere when it
condenses back
into liquid?
The moisture in the air is
condensed into a
water vapor and heated up, then it passes through the
liquid nicotine.