Water in the Atmosphere

The next block of material concerns water in the atmosphere. We will begin by describing the physics behind the important processes of evaporation and condensation. The concepts of relative humidity and dew point temperature will be explained. We will then show how the combination of air temperature, humidity, and winds relate to human comfort or discomfort and what is meant by windchill temperature and heat index. Next the process of cloud formation will be described. This will lead us to severe weather development since the heat released as clouds form provides much of the the energy for thunderstorms, tornadoes, and hurricanes.

Water is the only substance that exists in all three phase states (gas, liquid, and solid) at the temperatures found on the Earth. The concentration of the invisible gas water vapor varies greatly from place to place, and from time to time. In warm tropical locations close to the surface, water vapor can be up to 4% of the atmospheric gases. In cold polar regions, there is just a trace amount.

Water vapor is extremely important in the atmosphere because:

• It transforms into both liquid and solid cloud particles that grow and fall to Earth as precipitation.
• Releases large amounts of heat - called latent heat when it changes from vapor into water or ice. Latent heat is an important source of energy, especially for storms.
• Water vapor strongly absorbs infrared radiation, making it an important gas in the Earth's heat-energy balance. In fact water vapor is the largest contributor to the greenhouse effect on Earth.

Phase Changes of Water

The diagram below shows the energy transfers that occur as water changes phase. Water vapor has the highest internal energy per gram of water, followed by liquid water, and then ice. Any phase change from a lower to a higher internal energy state requires the addition of energy, while any phase change from a higher to a lower internal energy state involves a release of energy. The energy that is added or removed as water changes phases is called latent heat. Latent literally means "hidden". In this context it means that although energy must be added to liquid water to make it evaporate (liquid to gas), there is no measurable change in the temperature of the water. (When the water condenses, gas to liquid, the same amount of energy is released with no measurable change in temperature of the water). Energy which is used to change the measured temperature of a substance is called sensible heat. For example, to raise the temperature of liquid water from 20°C to 30°C requires the addition of sensible heat and to lower the temperature of liquid water from 30°C to 20°C requires the removal of sensible heat.

Deposition 680 cal/g Energy Released to environment (heating)
	Freezing 80 cal/g Melting		Condensation 590 cal/g Evaporation
Energy taken from Environment (cooling) Sublimation 680 cal/g

The calorie (cal) is a physical unit for measuring energy. It is defined as the amount of energy required to raise the temperature or one gram of liquid water by 1 degree Celsius. Notice from the diagram above how this compares to the tremendous amount of energy required or released per gram of water that is undergoing phase changes.

The processes of melting, evaporation, and sublimation absorb energy. This added energy causes the molecules to change their bonding pattern. In the Earth system, this energy must be supplied by the surrounding environment. Thus, these phase changes result in cooling of the surrounding environment.

The energy absorbed is latent heat and goes back to the environment when the phase changes reverse. In the Earth system, this energy is released to the surrounding environment. Thus, condensation, freezing, and deposition result in warming the surrounding environment.

In the atmosphere, phase changes between liquid and gas are the most important. Make sure that you understand that evaporation of water results in cooling of the surrounding environment and that condensation of water results in warming the surrounding environment.