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Sagot :
The air inside the packet can eventually reach saturation if we are to generate a cloud. The relative humidity is 100 percent at saturation.
- Because pressure lowers with height, air expands as it climbs. The temperature of the parcel drops as kinetic energy is changed to potential energy, and the relative humidity rises.
- The scientists came to the conclusion that temperature and humidity are inversely related to cloud cover. In other words, humidity increases with cloud cover, and temperature drops with cloud cover.
- The amount of water vapor present in the atmosphere determines the likelihood of cloud formation (and precipitation). Risen air becomes more relative humid as it cools. Once the temperature reaches the dew point and the relative humidity reaches 100%, a cloud will eventually develop.
To know more about cloud formation, kindly click on the link below :
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