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Cloud Formation Ingredients Required for Clouds: Water vapor (water as a gas) Cooling (change of the state: from gas to liquid or ice) CONDENSATION A surface for water vapor to condense on (condensation nuclei) How does the water get into the air? T E E T T By evaporation and transpiration E CONDENSATION Sunlight causes water to evaporate into the atmosphere. This air containing the water vapor is heated at the surface of the earth and rises. As the air rises, it cools and the water vapor condenses on some form of particulate matter such as dust, ash, or smoke to form clouds. The particulate matter are called Condensation Nuclei. Condensation on spider webs. Views of early morning fog in Indiana Importance of Clouds • So, what is a cloud? It is a thick mass of suspended water drops or ice crystals. • What do clouds tell us? The presence of clouds in the sky is one type of signal to meteorologists that there will be changes in the weather. Predicting the weather requires the understanding of the different types of clouds Cloud droplet formation • If the air temperature cools below the dew point, water vapor will tend to condense and form cloud/fog drops. • As with dew and frost, cloud drop formation prefers to condense on a surface of some sort - we call these particles cloud condensation nuclei. Without these particles clouds would not form. • Terrestrial Sources – Dust/sand/dirt particles – Smoke - volcanic, fires, and pollution – Pollens and spores • Oceanic Sources – Sea Salts Typical sizes Dew • Surfaces cool strongly at night – Strongest on clear, calm nights • If a surface cools below the dew point, water condenses on the surface and dew drops are formed Frost • If the temperature is below freezing, the dew point is called the frost point • If the surface temperature falls below the frost point water vapor is deposited directly as ice crystals • The resulting crystals are known as frost, hoarfrost, or white frost What factors result in cloud formation? 1. The air must rise 2. As the air rises, it encounters less pressure. The air molecules expand and cool (Adiabatic Cooling) 3. When the air is cooled to the dew point temperature condensation occurs and clouds begin to form What causes the air to rise? • Forced up over a mountain range Air rising and cooling to the dew point by expansion (adiabatic cooling) Pictures from the National Audubon Society Field Guide to Weather What causes the air to rise? • Convection current The Sun heating the ground, which then heats the air above, which then rises due to convection (is less dense than the cooler air surrounding it.) What causes the air to rise? • A mass of relatively low density is forced up and over a mass of cooler, more dense air This happens at the boundaries between AIR MASSES AIR MASS: A region of air that has similar temperature and moisture. Fronts: boundary that separates 2 different air masses 4 Types of weather fronts: Cold Front Stationary Front Warm Front Occluded Front Cold Front Fast moving cold air mass runs into a slow moving warm air mass and the thicker cold air slides under the lighter warmer air. A cold front symbol The direction that the teeth point indicate the direction the front is moving. Weather: showers and thunderstorms Warm Front Moving warm air mass collides with a slowly moving cold air mass and the warm air moves over the cold air. Warm Front symbol The directions that the bumps face is the direction the front is moving. Weather: fog, rain or snow Stationary Front Cold air mass and warm air mass meet, but neither air mass has enough force to move the other air mass. Stationary Front Symbol blue triangles point in the direction of the warmer air Occluded Front Warm air mass is caught between two cooler air masses and the thicker cold air masses move underneath the thinner warm air mass and push it upward. Occluded front symbol The directions that the bumps face is the direction the front is moving. Weather: rain, possible thunderstorms Which types of fronts can you find on this map?