What are three steps in the atmospheric water cycle?

The atmospheric water cycle encompasses the processes through which water moves within the atmosphere and between the Earth and its surroundings. The correct three steps—evaporation, condensation, and precipitation—represent fundamental stages in this continuous cycle.

Evaporation is the process where water transitions from a liquid state to a gaseous state as it absorbs heat from the environment. This process is critical because it is the primary means by which water enters the atmosphere.

Following evaporation, the water vapor rises and cools as it ascends, leading to condensation. During condensation, water vapor loses energy and transforms back into liquid droplets, forming clouds. This step is vital because it contributes to cloud formation and ultimately the return of water to the ground.

The cycle concludes with precipitation, which is when water droplets in clouds become heavy enough to fall back to the Earth's surface as rain, snow, sleet, or hail, thus reintroducing water into the environment.

While the other choices contain relevant terms and processes related to weather and hydrology, they do not accurately represent the primary steps in the water cycle. Transpiration, for example, involves the release of water vapor from plants but is part of the process rather than a distinct step. Similarly, rain, dew, and snow