Water in the Air Air has water vapor

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Water in the Air

Water in the Air

Air has water vapor in it. • Humidity- is the measure of water vapor

Air has water vapor in it. • Humidity- is the measure of water vapor in the air

Temperature affects how much water vapor the air can hold. • Warm air can

Temperature affects how much water vapor the air can hold. • Warm air can hold more water vapor than

Relative Humidity • Relative humidity is a ratio of how much water vapor the

Relative Humidity • Relative humidity is a ratio of how much water vapor the air is holding to how much water vapor it is capable of

 • Study the graph. • As the temperature increases, what • The same

• Study the graph. • As the temperature increases, what • The same amount of happens to the water vapor is in the percent of relative air. humidity? Does it • The air is shown at increase or decrease? different temperatures.

How to measure relative humidity: • A hygrometer measures relative humidity.

How to measure relative humidity: • A hygrometer measures relative humidity.

A psychrometer is a simple type of hygrometer. • A psychrometer is made of

A psychrometer is a simple type of hygrometer. • A psychrometer is made of 2 thermometer s. One is normal (dry bulb). One has a wet wick on the end (wet

The wet and dry bulb readings are compared using a table.

The wet and dry bulb readings are compared using a table.

evaporation • Evaporation is when liquid water becomes water vapor. • Water changes from

evaporation • Evaporation is when liquid water becomes water vapor. • Water changes from liquid to gas.

condensation Condensation is when water vapor becomes liquid water. Water changes from gas to

condensation Condensation is when water vapor becomes liquid water. Water changes from gas to liquid.

Dew point When air becomes cooler, it may reach a temperature where the air

Dew point When air becomes cooler, it may reach a temperature where the air can no longer hold its water in vapor form. At that point condensation occurs. That temperature is called the dew point.

Air is saturated… • …when the relative humidity is 100%. • If the air

Air is saturated… • …when the relative humidity is 100%. • If the air continues to cool, condensation occurs.

Examples of condensation: • Air in direct contact with your cold glass of ice

Examples of condensation: • Air in direct contact with your cold glass of ice water

Examples of condensation: • Air during the night can cool below saturation and reach

Examples of condensation: • Air during the night can cool below saturation and reach its dew point.

Examples of condensation: • Condensatio n on small particles of dust in the atmosphere

Examples of condensation: • Condensatio n on small particles of dust in the atmosphere forms clouds.

Examples of condensation: • Contrails are caused by water condensing on particles from the

Examples of condensation: • Contrails are caused by water condensing on particles from the exhaust of jets.

precipitation • Warm moist air rises and cools. • Condensation in the atmosphere forms

precipitation • Warm moist air rises and cools. • Condensation in the atmosphere forms clouds. • Eventually the condensation becomes too heavy to cling to dust particles in the air. • Rain, snow or sleet is the result.

barometer • A barometer measures air pressure. • When air pressure drops, warmer air

barometer • A barometer measures air pressure. • When air pressure drops, warmer air is rising and precipitation is predicted.

ASSIGNMENT • Look at current weather conditions in your area. • Find the •

ASSIGNMENT • Look at current weather conditions in your area. • Find the • Temperature • Relative humidity • Dew point • Barometric pressure (air