ALL clouds are made out of water drops, though some clouds like cirrus are made of ice.
Water condenses to form clouds when warm air rises, cools, and reaches its dew point—the temperature at which it can no longer hold all its water vapor. As the air cools, the water vapor condenses into tiny water droplets or ice crystals around particles like dust or smoke in the atmosphere, creating clouds.
Yes, water vapor is present in the atmosphere at all times, including nighttime. The amount of water vapor in the air can vary depending on factors such as temperature, humidity, and weather conditions.
Water vapor is the gaseous state of water present in the atmosphere, and it serves as the primary source for all clouds. As warm air rises, it cools and the water vapor condenses into tiny water droplets or ice crystals, forming clouds. This process is essential for the water cycle and contributes to weather patterns and precipitation. Essentially, without water vapor, clouds would not form, and weather as we know it would not exist.
Yes, if all the water has turned into water vapor, the temperature of the system could rise again if additional heat is introduced. Water vapor can absorb heat, and if the surrounding environment provides enough energy (like from the sun or a heat source), the temperature of the vapor can increase further. This process is a key component of the water cycle and affects weather patterns.
Not much. When the exhaust pipe is cold, water vapor will condense as the exhaust cools on the pipe. After the pipe heats up, the vapor will not condense. Remember that the combustion of hydrocarbon fuel produces both carbon dioxide AND water vapor as a normal part of the process. All gasoline engines produce water vapor and all water vapor condenses if the exhaust pipe is cool.
The temperature at which water begins to condense out of the air is called the dew point. It is the point at which air reaches full saturation and can no longer hold all of its water vapor, leading to condensation.
Rain is part of the water cycle and occurs under many varied conditions, all of which may condense liquid water from gaseous water vapor.
Water vapor from the atmosphere condenses to form clouds. When the air cools, it can no longer hold all the moisture it contains, causing the water vapor to condense into tiny water droplets or ice crystals, which then come together to form clouds.
Fog is a type of low-lying cloud that forms when water vapor in the air condenses into tiny water droplets. This happens when the air near the ground cools down to the point where it can no longer hold all the water vapor it contains, causing the vapor to condense into visible droplets that we see as fog.
The term is "dew point." It represents the temperature at which air becomes saturated with water vapor and can no longer hold all the moisture, leading to condensation on surfaces.
When water vapor condenses, it gives off energy or heat. That heat drives hurricanes and all other storms associated with rain. When the Ocean is warm, more water can evaporate. Then when the water vapor rises to the clouds, more water vapor can condense and provide heat, rain, and wind to make the hurricane stronger. If the ocean is cooler, less water can evaporate. Then, less water vapor can condense. The hurricane will get weaker. Very few hurricanes form in winter and those that do are quite weak.
The weather condition when water vapor condenses near the ground is fog. Fog forms when the air near the ground cools to the point where it can no longer hold all the water vapor it contains, causing the water vapor to condense into tiny water droplets that create the misty appearance of fog.
When cooler air cannot retain all its vapor, saturation occurs and excess water vapor will condense into liquid water droplets or ice crystals. This process leads to the formation of clouds, fog, or precipitation, depending on the temperature and altitude of the air.
Water condenses when warm, moist air cools down and reaches its dew point temperature. At this point, the air cannot hold all the water vapor it contains, causing it to condense into liquid water droplets. This process typically occurs when the air comes into contact with a cooler surface.
Water vapor in the air condenses into liquid water when the air is cooled below its dew point temperature, which is the temperature at which the air becomes saturated and can no longer hold all the moisture it contains as vapor. This causes the water vapor to turn into liquid droplets, forming clouds, fog, or dew.
If all the water vapor in the Earth's atmosphere were to condense and fall to the ground, it would cover the globe with about 1 inch (2.5 cm) of water. This would equate to approximately 1/25th of an inch (1 mm) if evenly distributed over the entire surface of the Earth.