The water goes in the air and forms into water vapor which turns into clouds.
Evaporated water rises into the atmosphere as water vapor due to heat from the sun. As the warm, moist air rises, it cools and condenses to form clouds. This process is part of the water cycle.
water vapour go up into the clouds as a gas causing the clouds to get heavy thus releasing water droplets
Water vapor rises in the atmosphere due to evaporation and warming of the air, which causes the vapor to become less dense and buoyant. As the air rises, it cools and condenses, forming clouds. When the water droplets in the clouds become too heavy to remain suspended, they fall as precipitation, such as rain.
Clouds are actually composed of tiny water droplets or ice crystals that have condensed in the atmosphere. These droplets are formed when water vapor in the air cools and condenses around particles called condensation nuclei. Evaporation is the process by which water changes from a liquid to a gas, but clouds are formed through condensation.
When water boils, it turns into water vapor or steam. This water vapor rises into the air and eventually dissipates.
Water vapor triggers convection currents that can form clouds.
When water boils, bubbles form due to the release of water vapor from the liquid. These bubbles contain water vapor, not air. The water itself does not disappear; it is transformed into water vapor, which you see as bubbles.
The water goes in the air and forms into water vapor which turns into clouds.
Dry what? Perhaps the water is evaporated, and becomes vapor in the air.
Warmer air has higher saturation mixing ratios then cold air does. So therefore because of this 100% humidity in cold air is not 100% humidity in warmer air. The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
The water is converted to water vapor and is carried out through the dryer vent by the air that flows through the machine.
The presence of water vapor decreases as altitude increases because the cooler temperatures at higher altitudes cause the water vapor to condense into clouds or rain, reducing the overall amount of water vapor in the air. Additionally, the air is thinner at higher altitudes, which limits the amount of water vapor that can be held in the atmosphere.
Water vapor in the air returns to the surface through the process of condensation, where the vapor cools and turns back into liquid water. This can happen when the temperature drops, causing the vapor to condense and form clouds, eventually leading to precipitation in the form of rain or snow that falls back to the Earth's surface.
The mistiness inside a beaker can be due to condensation of water vapor when the temperature of the beaker is different from the surrounding air. This can occur when a warm beaker comes in contact with cooler air, causing water vapor in the air to condense on the inner surface of the beaker.
As air temperature increases, its ability to hold water vapor also increases. This relationship is known as the Clausius-Clapeyron relation, which states that warm air can hold more water vapor than cold air. Conversely, as air temperature decreases, its capacity to hold water vapor decreases, potentially leading to condensation or precipitation.
Yes, evaporation occurs when water from precipitation on land or bodies of water is heated by the sun and turns into water vapor, which then rises into the air. This water vapor eventually forms clouds and can lead to more precipitation through the water cycle.