The K M Links Game - December 2024 Week...
Quizzes & Puzzles5 mins ago
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For more on marking an answer as the "Best Answer", please visit our FAQ.d g is qite right, if you have ever seen time-lapse photography of clouds, especially,say, over a mountain range, you will see the cloud accreting as the moist air rises above it's condensation level, and disappearing again ('ablating') as the airflow once more causes the condensed droplets to evaporate.
Then again, the water droplets that make up clouds would not form at all if it weren't for all the condensation nucleii that are present in the atmosphere. These are particles of dust, wind-blown soil, salt (from the seas and oceans), pollen, insects, volcanic particles, etc etc that are ever-present in our atmosphere - all of which are 'heavier than air' but are kept aloft by the winds and updraughts.
Think of it as 'muddy water' - given still conditions (a jar or bucket) it soon settles out - but in an ever moving river, the water stays 'muddy'.
Many times, as an air mass travels over a mountain range, water condensates, and rains out as the temperature drops. As condensation is a exothermic reaction, the temperature of the air mass increases so that the air mass is relatively warm and dry as it decends the other side of the mountain range. This describes the formation of a rain shadow.
As far as the muddy water analogy goes, moving water or turbulence is not always necessary to keep sediments suspended. Small clay particles can be held in suspension due to electrostatic interactions as a result of eletrical charges associated with the surfaces of the clay particles. I don't know if this mechanism is important in the atmosphere. Many airborn particles are electrically charged, but the air is not as viscous as water.