1. Classwork Students will take turns reading a paragraph and another student will summarize for the group what was just read. After reading the section, all students will work on the Thinking It Through and the Test Practice questions. After 15-20 minutes, students will present their lesson to the class: – Summarize the lesson and highlight the major concepts. – Be prepared to complete the reviews with the class tomorrow.

2. Lesson 13 – Heat and Weather Patterns Weather and climate are different process Weather is a process in the atmosphere that changes over short periods of time Climate is the weather that is in the place most of the time or over a long period of time. Energy from the sun no matter where it goes turns into heat 51 percent of solar radiation is absorbed into the ground Convection currents : Warm air a rises and cool air takes its place Density : the mass divided by volume You can see some of the energy or solar radiation that reaches earth from the sun visible light is energy you can see It might be moist and rainy and dry another Weather is controlled by the suns radiation Some radiation bounces back in to space

3. Lesson 13 Land absorbs radiation from the sun – Slower than water. – Faster than water – At the same rate as water – Almost never

4. Lesson 13 Land absorbs radiation from the sun – Slower than water. – Faster than water – At the same rate as water – Almost never

5. Lesson 13 In the atmosphere, what happens in a convection current? – Cool air and warmer air both rise – Cool air and warmer air both fall – Cool air rises and warmer air falls – Cool air falls and warmer air rises

6. Lesson 13 In the atmosphere, what happens in a convection current? – Cool air and warmer air both rise – Cool air and warmer air both fall – Cool air rises and warmer air falls – Cool air falls and warmer air rises

7. Lesson 13 What does solar radiation produce on Earth? – Light – Heat – Land – water

8. Lesson 13 What does solar radiation produce on Earth? – Light – Heat – Land – water

9. Lesson 13 In which direction does a sea breeze move? – Toward the land – Toward the sea – Up – down

10. Lesson 13 In which direction does a sea breeze move? – Toward the land – Toward the sea – Up – down

11. Lesson 13 How are climate and weather alike? – They both occur over short periods of time – They both occur over long periods of time – They both are affected by radiation from the sun – They are both caused by the even heating of Earth’s surface

12. Lesson 13 How are climate and weather alike? – They both occur over short periods of time – They both occur over long periods of time – They both are affected by radiation from the sun – They are both caused by the even heating of Earth’s surface

13. Lesson 14 – Global Wind Systems and Weather Events Unique heating of earth produces global winds Sunlight hits the equator directly High density = high pressure Low density= low pressure Air moves from high pressure to low pressure Tornados produces fastest winds on earth Cold air is denser then warm air Tornados are tunnels of low pressure air Low density air rises quickly High pressure air over the poles sinks and moves toward low pressure air over the equator

14. Lesson 14 What combination produces global winds? – Low-pressure polar air and low-pressure equatorial air – Low-pressure polar air and high-pressure equatorial air – High-pressure polar air and high-pressure equatorial air – High-pressure polar air and low-pressure equatorial air

15. Lesson 14 What combination produces global winds? – Low-pressure polar air and low-pressure equatorial air – Low-pressure polar air and high-pressure equatorial air – High-pressure polar air and high-pressure equatorial air – High-pressure polar air and low-pressure equatorial air

16. Lesson 14 What is MAINLY responsible for the unequal heating of Earth’s surface? – The distance of the sun from different parts of Earth – The angle at which sunshine strikes Earth’s surface – The material on Earth’s surface – Changes in the amount of energy the sun puts out

17. Lesson 14 What is MAINLY responsible for the unequal heating of Earth’s surface? – The distance of the sun from different parts of Earth – The angle at which sunshine strikes Earth’s surface – The material on Earth’s surface – Changes in the amount of energy the sun puts out

18. Lesson 14 What makes global winds curve rather than move in straight lines? – Differences in air pressure – Differences in density – Differences in temperature – Earth’s rotation on its axis

19. Lesson 14 What makes global winds curve rather than move in straight lines? – Differences in air pressure – Differences in density – Differences in temperature – Earth’s rotation on its axis

20. Lesson 14 What properties of air near the ground are likely to produce a thunderstorm? – Moist, low pressure – Dry, low pressure – Moist, high pressure – Dry, high pressure

21. Lesson 14 What properties of air near the ground are likely to produce a thunderstorm? – Moist, low pressure – Dry, low pressure – Moist, high pressure – Dry, high pressure

22. Lesson 14 Which combination of properties describes cold air? – High density and low pressure – Low density and low pressure – High density and high pressure – Low density and high pressure

23. Lesson 14 Which combination of properties describes cold air? – High density and low pressure – Low density and low pressure – High density and high pressure – Low density and high pressure

24. Lesson 15 – Moisture and Weather Patterns Tropical cyclones are large and very powerful they also have spinning winds. Tropical cyclones that are formed in the Atlantic Ocean and the east Pacific Ocean they are called hurricanes. The tropical cyclones can make 1,000 to 3,000 kilometers and may last up to about 2 weeks. The eye of the storm forms in the center, has low air pressure, and it’s calm. Tropical storms are born over warm water near the equator the water rises and produces an area of low pressure called tropical depression The air in the center of a depression in the northern hemisphere begins to spin in a counterclockwise direction There are many other names for tropical cyclones such as typhoons (western pacific ocean), hurricanes (Atlantic ocean), and monsoon (India) The center of the eye is moist warm air

25. Lesson 15 What is the source of a hurricane’s energy? – Warm, moist air evaporating from the sea – cool, moist air evaporating from the sea – Warm, dry air evaporating from the sea – Warm, moist air condensing from the sea

26. Lesson 15 What is the source of a hurricane’s energy? – Warm, moist air evaporating from the sea – cool, moist air evaporating from the sea – Warm, dry air evaporating from the sea – Warm, moist air condensing from the sea

27. Lesson 15 The general name for a powerful tropical storm is a – Tropical depression – Tropical cyclone – Hurricane – typhoon

28. Lesson 15 The general name for a powerful tropical storm is a – Tropical depression – Tropical cyclone – Hurricane – typhoon

29. Lesson 15 Where are tropical storms born? – Over water near Earth’s poles – Over land near Earth’s poles – Over water near the equator – Over land near the equator

30. Lesson 15 Where are tropical storms born? – Over water near Earth’s poles – Over land near Earth’s poles – Over water near the equator – Over land near the equator

31. Lesson 15 What happens when moist air rises high into the sky? – It cools and evaporates – It cools and condenses – It warms and evaporates – It warms and condenses

32. Lesson 15 What happens when moist air rises high into the sky? – It cools and evaporates – It cools and condenses – It warms and evaporates – It warms and condenses

33. Lesson 15 The eye of a hurricane has – Low pressure and high winds – Low pressure and no winds – High pressure and high winds – High pressure and no winds

34. Lesson 15 The eye of a hurricane has – Low pressure and high winds – Low pressure and no winds – High pressure and high winds – High pressure and no winds