It takes the water content of about 1,000,000 cloud droplets to form a single raindrop.
The tiny particles called cloud droplets are what give rise to all the well-known, observable, non-precipitating clouds that are discussed in Chapter 1 (stratus, stratocumulus, cumulus, altostratus, altocumulus, and cirriform clouds).
When airborne water vapor in the form of visible water droplets or ice crystals condenses, clouds are created. In order for this to occur, the air parcel must be saturated, meaning that it must be unable to keep all the water it contains in vapor form, causing it to begin condensing into a liquid or solid form.
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