it explodes man
The concentration of water vapor in the atmosphere decreases as altitude increases. Most planes fly near the tropopause since there's less water vapor and, therefore, weather there.
it condenses
it will precipitate
The cool atmosphere condenses the rising water vapor and causes it to fall back to Earth
Clouds, fog.
The higher you go, the colder it gets. The colder it gets, the less water vapor can remain in the air. That's the reason it rains on the windward side of mountain ranges. Warm, moist air gets pushed up and the rain condenses.
When the sun heats the Earth's water, it evaporates and turns into water vapor. Water vapor rises into the atmosphere where it can eventually condense to form clouds and then fall back to Earth as precipitation. This process is known as the water cycle.
transpiration
The amount of water vapor in the atmosphere can vary based on factors like temperature, humidity, and weather patterns. Warmer air can hold more water vapor than cooler air, so regions with higher temperatures tend to have more water vapor. Additionally, changes in humidity levels and the presence of weather systems like storms can also affect the amount of water vapor in the atmosphere.
Water in the atmosphere stays there as water vapor, or it condenses and falls as rain, snow, hail, etc.
Water in the atmosphere stays there as water vapor, or it condenses and falls as rain, snow, hail, etc.
particles of water vapor collect dust around the air causing it to rise higher until it reaches the atmosphere