the height at which the condensation starts in a rising air parcel is called condensation limit.
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In a Rising Parcel of Air that's NOT Saturated. No change in water vapor and temperature decreases. RH = mixing ratio/saturation mixing ratio Relative humidity increases. When the Air is Saturated. Once the air is saturated, condensation or deposition occurs and cloud begins to form.
In a Rising Parcel of Air that's NOT Saturated. No change in water vapor and temperature decreases. RH = mixing ratio/saturation mixing ratio Relative humidity increases. When the Air is Saturated. Once the air is saturated, condensation or deposition occurs and cloud begins to form.
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