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Water and Wind in Earth’s Atmosphere
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Winds What causes this?
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What is Wind? Wind is the horizontal movement of air from an area of high pressure to an area of low pressure. Larger difference in pressure = stronger wind Differences in air pressure are caused by unequal heating in the atmosphere. As cooler, denser air sinks, warm, less dense air is forced to rise.
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Measuring Wind Winds are described by their direction and speed:
A wind vane determines wind direction. An anemometer measures wind speed. The name of the wind tells you the direction it is blowing from a west wind blows from the west toward the east.
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Local Winds Local winds are winds that blow over short distances and are caused by the unequal heating of Earth’s surface within a small area. A sea breeze is a local wind that blows from a lake or ocean toward land Since land is heated faster than a body of water, the air above the land gets warmer and rises, allowing cooler air from the ocean to move underneath the warm air.
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Humidity Humidity: how much H2O vapor is in the air.
What can hold more water? warm or cold air? Relative humidity: the % of water vapor in the air compared to the maximum amount of water vapor the air can hold at a given temperature Psychrometer: device used to measure relative humidity, by comparing a “dry” temperature and a “wet” temperature.
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Cloud Formation Clouds form when H2O vapor condenses into liquid water or ice crystals. 2 conditions needed: 1. cooling of the air 2. particles in the air for H2O vapor to condense around
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Clouds are classified by:
Shape Cumulus – puffy Cirrus – thin, wispy Stratus – flat, layered B. Altitude/weather 1. Cirro – high 2. Alto – mid-level 3. Nimbo – rain producing
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Guess the Clouds!
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