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WEATHER PATTERNS. Lesson 1 How Does Air Move? Layers of Air Convection Currents Wind Patterns.

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Presentation on theme: "WEATHER PATTERNS. Lesson 1 How Does Air Move? Layers of Air Convection Currents Wind Patterns."— Presentation transcript:

1 WEATHER PATTERNS

2 Lesson 1 How Does Air Move? Layers of Air Convection Currents Wind Patterns

3 Air is a mixture of gases in constant motion Differences in air temperatures create winds. About.8 of the air is nitrogen and about.2 is oxygen. A very small part of the air is carbon dioxide, water vapor, and other gases. There are five layers of Earth’s atmosphere: Troposphere- Altitude: about 8–15 kmTemperature: –55°C Stratosphere - Altitude: about 50 kmTemperature: 0°C Mesosphere - Altitude: about 85 kmTemperature: –90°C Thermosphere - Altitude : about 320 km Large Temperature Fluctuations Exosphere - Altitude: about 600 kmTemperature: 1700°C As you go up through the five layers, temperatures and air pressure change. Air pressure decreases as you go up through the atmosphere. This decrease happens because the gas particles in the air get farther apart and there is less air above you. Layers of Air

4 Land gets warm more quickly in sunlight than water does. At night, land cools faster than water. This causes the air above the land and water to have different temperatures. Winds, storms, and all sorts of weather happen because of the different air temperatures. Convection currents are also caused by different air temperatures. In convection currents, gases or liquids rise and sink in a circular path. In cool air, gas particles are closer together than in warm air. Every liter of cool air is heavier than every liter of warm air. When the two kinds of air are next to each other, the cool air will sink and force the warm air to rise. Convection Currents

5 Convection Currents cause daily patterns of clouds, wind, rain, and air pressure

6 Wind Patterns Six huge convection currents form in the air above Earth. One reason they form is that tropical regions get warmer than other parts of Earth. The moving of the huge convection currents combines with the spinning of Earth to cause regional surface wind patterns. Jet streams are high above the ground between these huge convection currents. A jet stream is a band of very fast wind formed by the different temperatures between the convection currents.

7 Lesson 2 Properties and Kinds of Air Masses Four Air Masses When Air Masses Meet

8 Properties and Kinds of Air Masses Air that stays over an area for some time takes on properties of that area and becomes an air mass. An air mass is a large body of air with similar properties all through it. The most important properties are temperature and amount of water vapor. An air mass keeps its original properties for a while as it moves. The kind of weather you have at any time is because of the air mass in your area.

9 Four Air Masses 1) Maritime Tropical Air Humid air has lots of moisture. Over tropical oceans or rainforests, an air mass becomes warm and very humid because water can easily evaporate there 2) Maritime Polar Air Even though the ocean near the poles is cold, water vapor evaporates into the air. An air mass forming over the poles is cold and moist.

10 3) Continental Tropical Air A large hot desert can cause the air above it to be warm and fairly dry. 4)Continental Polar Air The land near the poles is not very moist. So, the air mass from this area is cold and fairly dry

11 When Air Masses Meet A front is a boundary between two air masses. A cold front brings colder air into an area. A warm front brings warmer air into an area. Rising air at fronts often causes rain or snow.

12 Lesson 3 Thunderstorms Tornados Hurricanes

13 Thunderstorms Stage One- strong, quickly upward currents of moist air. Clouds grow. Stage Two- Precipitation starts to fall, which pulls air down with it. There is upward and downward air movement. Stage Three- All air currents are moving downward. Clouds get smaller as more precipitation falls. Lightening is a large electrical spark moving between areas of opposite electrical charge.

14 Tornados Layers of wind form from wind moving at various speeds in different directions. A column of spinning air is formed between the layers of wind. Upward winds push one end of the column up and downward winds push the other end down creating a funnel called a tornado. Tornados form quickly and last only a few minutes.

15 Hurricanes Hurricanes get their energy from warm ocean water. Hurricane winds are not as fast as a tornado but they can cause more damage because they can last for days and they are very large storms.

16 Lesson 4 Collecting Data Weather Forecasts Weather Maps

17 Collecting Data A weather system is described in terms of temperature, moisture, clouds, precipitation, air pressure, wind speed, and wind direction. Various instruments are used for forecasting the weather: – A barometer shows air pressure – An anemometer measures wind speed – A hydrometer measures the moisture in the air – A rain gauge measures how much rain has fallen – A radar measures winds and precipitation inside a storm

18 Weather Forecasts Weather forecasters observe many patterns of weather change. They use this information to make inferences that help them to predict what weather will be like in the future.

19 Weather Maps Forecasters use weather maps to show current weather conditions and their predictions.

20 Lesson 5 Weather and Climate Climate is the average weather conditions over a long period of time, usually 30 years Climate includes such things as average amount of precipitation, average temperature, and how much the temperature changes over the year. Fossils have helped scientists make assumptions about ancient climates


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