Lesson 2-1 A high-pressure system is a large body of circulating air with high pressure at its center and lower pressure outside of the system.high-pressure.

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Presentation transcript:

Lesson 2-1 A high-pressure system is a large body of circulating air with high pressure at its center and lower pressure outside of the system.high-pressure system Pressure Systems

Lesson 2-1 A low-pressure system is a large body of circulating air with low pressure at its center and higher pressure outside of the system.low-pressure system Pressure Systems (cont.)

Lesson 2-2 Air masses are large bodies of air with distinct temperature and moisture characteristics.Air masses An air mass forms when a large high pressure system lingers over an area for several days. As a high pressure system comes in contact with Earth, the air in the system takes on the temperature and moisture characteristics of the surface below it. Air Masses

Lesson 2-2 Five main air masses impact climate across North America. Air Masses (cont.)

Lesson 2-2 Air masses are classified by their temperature and moisture characteristics. Continental air masses form over land. Maritime masses form over water. Air Masses (cont.)

Lesson 2-2 Tropical air masses form in the warm equatorial regions. Polar air masses form over cold regions. Arctic and antarctic air masses form near the poles, over the coldest regions of the globe. Air Masses (cont.)

Lesson 2-3 A weather front is a boundary between two air masses.front Changes in temperature, humidity, clouds, wind, and precipitation are common at fronts. Fronts

Lesson 2-3 When a colder air mass moves toward a warmer air mass, a cold front forms. Fronts (cont.)

Lesson 2-3 A warm front forms when lighter, warmer air moves toward colder, heavier air. Fronts (cont.)

Lesson 2-3 When the boundary between two air masses stalls, the front is called a stationary front. Fronts (cont.)

Lesson 2-3 When a fast- moving cold front catches up with a slow-moving warm front, an occluded or blocked front forms. Fronts (cont.)

Lesson 2-4 Thunderstorms have warm temperatures, moisture, and rising air, which may be supplied by a low- pressure system. Thunderstorms have a three-stage life cycle: the cumulus stage, the mature stage, and the dissipation stage. Severe Weather

Lesson 2-4 The cumulus stage is dominated by cloud formation and updrafts. After the cumulus stage, downdrafts, which are air currents moving vertically toward the ground, begin to form. Severe Weather (cont.)

Lesson 2-4 In the mature stage, heavy winds, rain, and lightning dominate the area. In the dissipation stage, updrafts stop, winds die down, lighting ceases, and precipitation weakens. Severe Weather (cont.)

Lesson 2-4 A tornado is a violent, whirling column of air in contact with the ground.tornado Tornadoes form when thunderstorm updrafts begin to rotate. Tornado Alley is the name given to the area of the central United States that experiences the most tornadoes. Severe Weather (cont.)

Lesson 2-4 An intense tropical storm with winds exceeding 119 km/h is a hurricane.hurricane Severe Weather (cont.) hurricane from Spanish huracan, means “tempest”

Lesson 2-4

A blizzard is a violent winter storm characterized by freezing temperatures, strong winds, and blowing snow.blizzard Severe Weather (cont.) What are examples of severe weather?

Lesson 2-4 The U.S. National Weather Service issues watches and warning for different types of severe weather. A watch means that severe weather is possible. A warning means that severe weather is already occurring. Severe Weather (cont.)