What is a common outcome of high relative humidity in the atmosphere?

High relative humidity in the atmosphere is often associated with increased precipitation. When the air is saturated with moisture, it means that the atmosphere can hold a significant amount of water vapor. As this moisture accumulates, it can lead to cloud formation. Once the clouds reach a certain thickness, the water vapor in the clouds condenses into liquid droplets, resulting in precipitation such as rain, snow, or drizzle.

This relationship between humidity and precipitation is essential in understanding weather patterns. When relative humidity is high, it indicates that the air is near its capacity for moisture, creating conditions conducive for various types of precipitation to occur. This contrasts with conditions of low humidity, where the atmosphere is drier and less likely to produce rain or other forms of precipitation. Thus, high relative humidity is a key factor in the precipitation process.