a.
sublimation
b.
evaporation
c.
evapotranspiration
Water vapor enters the atmosphere through evaporation, where liquid water on the Earth's surface changes into a gas, and through transpiration, where water vapor is released from plants through their leaves.
Water enters the atmosphere through evaporation, where liquid water changes into water vapor due to heat energy. It also enters through transpiration, where water vapor is released into the air by plants through their leaves.
Water is added to the atmosphere through the processes of evaporation and transpiration. Evaporation occurs when water changes from liquid to vapor from bodies of water like oceans and lakes. Transpiration is the release of water vapor from plants through their leaves.
Water transfers into the atmosphere through processes like evaporation from bodies of water, such as oceans, lakes, and rivers, and transpiration from plants. Additionally, water can enter the atmosphere through sublimation from snow or ice directly into water vapor.
Water can enter the atmosphere through the process of evaporation, where liquid water changes into water vapor due to heat energy from the sun. Another way is through transpiration, where plants release water vapor through their leaves during photosynthesis.
water vapor and condensation
Water vapor enters the atmosphere through evaporation, where liquid water on the Earth's surface changes into a gas, and through transpiration, where water vapor is released from plants through their leaves.
Water enters the atmosphere through evaporation, where liquid water changes into water vapor due to heat energy. It also enters through transpiration, where water vapor is released into the air by plants through their leaves.
Water is added to the atmosphere through the processes of evaporation and transpiration. Evaporation occurs when water changes from liquid to vapor from bodies of water like oceans and lakes. Transpiration is the release of water vapor from plants through their leaves.
Water transfers into the atmosphere through processes like evaporation from bodies of water, such as oceans, lakes, and rivers, and transpiration from plants. Additionally, water can enter the atmosphere through sublimation from snow or ice directly into water vapor.
Water can enter the atmosphere through the process of evaporation, where liquid water changes into water vapor due to heat energy from the sun. Another way is through transpiration, where plants release water vapor through their leaves during photosynthesis.
Water in the atmosphere can exist as water vapor, which is an invisible gas. It can also form clouds, which are condensed water droplets or ice crystals. Lastly, water in the atmosphere can fall back to the Earth's surface in the form of rain, snow, sleet, or hail.
Water vapor enters the earth's atmosphere in mountain regions through evaporation from bodies of water and vegetation, as well as through sublimation from snow and ice. Additionally, the orographic lift effect can cause air to rise and cool, leading to condensation and the formation of clouds.
Water moves through the atmosphere in the form of vapor through evaporation from oceans, lakes, rivers, and plants. It also moves through the atmosphere as clouds and precipitation through processes like condensation and precipitation.
In atmospheric science, the degrees of freedom of water vapor are important because they determine the behavior and properties of water vapor in the atmosphere. The degrees of freedom refer to the number of ways a molecule can move or vibrate independently. In the case of water vapor, the degrees of freedom affect its ability to absorb and release energy, which in turn influences weather patterns and climate dynamics. Understanding the degrees of freedom of water vapor helps scientists predict and study atmospheric processes more accurately.
They have the same chemical composition of H2O.
To saturate the air with water vapor, you can lower the temperature to it's dew point, and leave out water to be evaporated.