Atmosphere Glencoe. Name

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Atmosphere 2005 Glencoe Name

Note-taking Worksheet Atmosphere Section 1 Earth s Atmosphere A. thin layer of air that protects the Earth s surface from extreme temperatures and harmful Sun rays B. Atmospheric makeup mixture of gases,, and liquids 1. Early atmosphere was much different than today. a. Volcanoes produced nitrogen and carbon dioxide, but little. b. More than 2 billion years ago began producing oxygen. c. Eventually oxygen formed an layer that protected Earth from harmful rays. d. plants and diverse life forms developed. 2. Atmospheric include nitrogen (78%), oxygen (21%), carbon dioxide, water vapor, and argon. a. Atmosphere is changing with the introduction of pollutants: increasing human energy use is increasing the amount of. b. Pollutants mix with oxygen and other chemicals to form. 3. include dust, salt, and pollen. 4. include water droplets and droplets from volcanoes. C. main layers of the atmosphere 1. layers a. Lowest layer, where humans live, is the, which extends about 10 km up, and contains most of the water vapor and gases. b. Extending from 10 km to 50 km above Earth, the contains ozone. 2. layers a. extends from 50 km to 85 km and is the layer in which meteors are visible. b. Thickest part of atmosphere is from 85 km to 500 km and is called the for its high temperatures. c. Within the mesosphere and thermosphere is a layer of charged particles called the that can help carry radio waves. d. outer layer of atmosphere in which the space shuttle flies; has very few molecules D. molecules closer to the surface are more densely packed (at higher pressure) than those higher in the atmosphere because of the mass of gases pressing down from higher in the atmosphere. Atmosphere 29

Note-taking Worksheet (continued) E. in atmospheric layers 1. The troposphere is warmed primarily by the Earth s surface; temperature as altitude increases in this layer. 2. Temperatures as altitude increases in the stratosphere, particularly the upper portion because ozone absorbs energy from the Sun. 3. Temperatures with altitude in the mesosphere. 4. Thermosphere and exosphere are the first to receive the Sun s rays, so they are very F. about 19 km to 48 km above Earth in the stratosphere, this layer of 3-atom oxygen molecules (O 3 )protects the Earth from the Sun s harmful ultraviolet radiation 1. Life on Earth, as we know it, on it. 2. Pollutants called (CFCs) are destroying the ozone layer. a. CFCs are used in, air conditioners, aerosol sprays, and foam packaging. b. If these products develop a leak, CFCs can enter the. 3. The ozone layer has a large hole over. Section 2 Energy Transfer in the Atmosphere A. Some energy from the Sun is reflected back into, some is absorbed by the, and some is absorbed by and water on Earth s surface. B. energy that flows from an object with a higher temperature to one with a lower temperature 1. energy transferred in rays or waves 2. transfer of energy when molecules bump into each other through contact 3. transfer of heat by the flow of a material a. Molecules move closer together, making the air more dense, and air rises. b. Cold air, pushing up warm air, which then cools and sinks, pushing up more warm air. C. The cycle water moves back and forth between Earth s atmosphere and surface 1. Energy from the Sun causes water to from the hydrosphere, and rise as vapor. 30 Atmosphere

Note-taking Worksheet (continued) 2. Water vapor in the atmosphere can cool and return to liquid form through a. When water vapor condenses, clouds of tiny water may form. b. Water droplets collide to form larger. 3. As water drops grow, they fall back to Earth as. D. Earth s atmosphere is unique it holds just the right amount of the Sun s to support life. Section 3 Air Movement A. is the movement of air from an area of high pressure to an area of lower pressure. 1. Different areas of Earth receive different amounts of the Sun s. a. The equator s warm air, being less dense, is pushed upward by denser, air. b. The pole s cold air, being more, sinks and moves along Earth s surface. 2. The rotation of the Earth causes moving air and water to shift to the right north of the equator and left south of the equator B. Global winds wind patterns, caused by convection currents combined with the Coriolis effect, affect the world s 1. Near the equator, very little wind and daily rain patterns called the 2. Surface winds a. Between the equator and 30 latitude (north and south) are steady, blowing to the west. b. Between 30 and 60 latitude (north and south) the blow to the east, in the opposite direction of the trade winds. c. blow from northeast to southwest near the north pole and from southeast to northwest near the south pole. 3. Upper troposphere narrow belts of strong winds called a. Jet stream moves in the winter. b. Moves systems across the country C. Local wind systems affect weather 1. a convection current blows wind from the cooler sea toward warmer land during the day 2. at night, air moves off the land toward the water as the land cools more rapidly than the water Atmosphere 31

Determining If Air Has Mass Procedure 1. On a pan balance, find the mass of an inflatable ball that is completely deflated. 2. Hypothesize about the change in the mass of the ball when it is inflated. 3. Inflate the ball to its maximum recommended inflation pressure. 4. Determine the mass of the fully inflated ball. Hands-On Activities Mass of Ball When Completely Deflated Predicted Mass of Ball When Fully Inflated Analysis 1. What change occurs in the mass of the ball when it is inflated? 2. Infer from your data whether air has mass. Actual Mass of Ball When Fully Inflated Atmosphere 3

2 Laboratory Activity Temperature of the Air Air temperature is an important factor in the scientific study of weather. Air temperature affects air pressure and, thus, the type of weather that may occur. Differences in air temperature also cause winds. By studying the air temperature and weather at different times during the day, you may be able to predict how the air temperature will affect local weather. Strategy You will measure air temperature at different times during the day. You will measure air temperature at the same location each time. You will graph your results and compare your graph with those of your classmates. Materials Celsius thermometer (metal backed) graph paper Procedure 1. Select an outdoor site for taking air temperature readings. Make sure the site is an open shaded area. 2. Record the air temperature at this site three times each day for a week. Be careful to read the thermometer at the same times each day. Record data in Table 1. 3. Record additional weather factors, such as cloud cover, precipitation, and winds. Data and Observations Table 1 Date Time Temp ( C) Other 1. 2. 3. 1. 2. 3. 1. 2. 3. 1. 2. 3. 1. 2. 3. Hands-On Activities Atmosphere 11

Laboratory Activity 2 (continued) Hands-On Activities Graph your data showing temperature and time. Graph temperature on the vertical axis and time on the horizontal axis. Temperature Time Questions and Conclusions 1. Why did you take your air temperature readings in the shade instead of the Sun? 2. Describe any patterns in your air temperature graph. 3. Do these patterns agree with patterns observed by your classmates? Explain. 4. How can you explain the patterns in terms of solar energy absorbed by the land? Strategy Check Can you measure air temperature? Can you collect data for a week? Can you graph your data? 12 Atmosphere

Evaluating Sunscreens Lab Preview Directions: Answer these questions before you begin the Lab. 1. Why are terms like sunblock and waterproof misleading? Hands-On Activities 2. Why is it important to calculate the cost per milliliter of each brand of sunscreen? Without protection, sun exposure can damage your health. Sunscreens protect your skin from UV radiation. In this lab, you will draw inferences using different sunscreen labels. Real-World Question How effective are various brands of sunscreens? Materials variety of sunscreens of different brand names Goals Draw inferences based on labels on sunscreen brands. Compare the effectiveness of different sunscreen brands for protection against the Sun. Compare the cost of several sunscreen brands. Safety Precautions Data and Observations 1. 2. 3. 4. Brand Name SPF Cost per Milliliter Procedure 1. The Sun Protection Factor (SPF) tells you how long the sunscreen will protect you. For example, an SPF of 4 allows you to stay in the Sun four times longer than if you did not use sunscreen. Record the SPF of each sunscreen on the data table below. 2. Calculate the cost per milliliter of each sunscreen brand. 3. Government guidelines say that terms like sunblock and waterproof are misleading because sunscreens can t block the Sun s rays, and they do wash off in water. List misleading terms in the data table for each brand. Misleading Terms Atmosphere 5

(continued) Hands-On Activities Conclude and Apply 1. Explain why you need to use sunscreen. 2. Evaluate A minimum of SPF 15 is considered adequate protection for a sunscreen. An SPF greater than 30 is considered by government guidelines to be misleading because sunscreens wash or wear off. Evaluate the SPF of each sunscreen brand. 3. Discuss Considering the cost and effectiveness of all the sunscreen brands, discuss which brand you consider to be the best buy. Communicating Your Data Create a poster on the proper use of sunscreens, and provide guidelines for selecting the safest product. 6 Atmosphere

Directed Reading for Content Mastery Overview Atmosphere Directions: Complete the concept map using the terms in the list below. weather exosphere coldest air temperature ionosphere stratosphere 1. which is the region of space travel thermosphere which also contains the 2. The layers of the atmosphere are the mesosphere which has the 3. 4. troposphere which contains the in which ozone layer 5. occurs Atmosphere 15

Directed Reading for Content Mastery Section 1 Earth s Atmosphere Section 2 Energy Transfer in the Atmosphere Directions: Unscramble the terms in italics to complete the sentences below. Write the terms on the lines provided. 1. The layer of atmosphere that we live in is the oreeshroppt. 2. The most common gas in our atmosphere is gnoetrin. 3. The layer of atmosphere that contains the ozone layer is the rattsoreephs. 4. Harmful energy that comes from the sun is travelutoil triadiona. 5. Chemical compounds that pollute the atmosphere are frochrabonlorolucos. 6. Energy is transferred when molecules bump into one another in notonducci. 7. A cycle in which air is warmed, warm air rises, air is cooled, and cooled air sinks is a nocitecnov centurr. 8. All the water on Earth s surface is called the dropshyere. 9. The process of water vapor changing to a liquid is called cannedsitnoo. 10. When water changes from a liquid to a gas, it asprotavee. 16 Atmosphere

Directed Reading for Content Mastery Section 3 Air Movement Directions: Identify the illustrations below as showing a sea breeze or land breeze. Warm air Warm air Cool air Cool air 1. 2. Directions: Match each cause with the correct effect. Write the letter of the effect in the blank before the cause. Cause Effect 3. The equator receives more of the Sun s energy. 4. Warm air is less dense than cold air. 5. The poles receive less of the Sun s energy. 6. Cold air is more dense than warm air. 7. Warm air molecules are farther apart. 8. Earth rotates. a. Cold air sinks. b. Air near the equator is warmer. c. The Coriolis effect exists. d. Warm air rises. e. Warm air is less dense. f. Air near the poles is colder. Atmosphere 17

Key Terms Atmosphere Directions: Use the terms to complete the puzzle below. The letters in the dark, vertical box will spell a familiar term. Coriolis effect troposphere sea breeze ionosphere ozone layer jet stream radiation land breeze condensation hydrosphere 1 Directed Reading for Content Mastery 3 2 5 6 4 7 8 9 10 1. Part of atmosphere that protects Earth from harmful radiation 2. The transfer of energy that occurs when molecules bump into one another 3. Narrow belt of strong wind at high altitude 4. All the water on Earth s surface 5. The process of water vapor changing to a liquid 6. Layer of atmosphere closest to Earth s surface 7. A layer of charged particles above Earth 8. Constant movement of water between the atmosphere and Earth s surface. 9. Shifts the direction of free moving fluids such as air and water 10. A local wind system created during the day 18 Atmosphere

1 Reinforcement Earth s Atmosphere Directions: Answer the following questions on the lines provided. 1. Which atmosphere layer contains electrically charged particles that reflect radio waves? 2. In which atmosphere layer(s) does the temperature increase as altitude increases? 3. In which atmosphere layer(s) does the temperature decrease as altitude increases? Directions: Use the chart to answer questions 4 7. Gas Percent by volume A 78.09 B 20.95 Argon 0.93 Gas Helium Methane Krypton Percent by volume trace trace trace Carbon dioxide 0.03 Xeron trace C 0.0 to 4.0 Hydrogen Neon trace Ozone 4. What information does the chart show? 5. A, B, and C represent three different gases. What is A? How do you know? 6. What is B? How do you know? 7. What is C? How do you know? trace trace Atmosphere 23

2 Reinforcement Directions: Answer the following questions on the lines provided using information from the graph. 1. Why doesn t all radiation directed at Earth reach the surface? 2. What percent of radiation is lost before reaching Earth s surface? 3. What percent of radiation is lost after reaching Earth s surface? Energy Transfer in the Atmosphere What happens to radiation coming to Earth from the sun? Absorbed by Earth's surface 4. What factors in the atmosphere seem to have the greatest effect on the amount of radiation received from the Sun? 50% 5% Reflected by Earth's surface 25% 20% Absorbed by clouds and atmosphere Scattered by clouds and air Directions: Complete the chart using the correct terms and phrases from the chapter. Then answer the following questions on the lines provided. Types of heat transfer 5. Radiation 6. Conduction 7. Convection produced by produced by produced by How they are produced 8. If you put a frying pan on a burner on a stove and turn the burner on, the bottom of the frying pan gets hot. What type of heat transfer has occurred? 9. When you get in a closed car on a sunny day and the temperature inside is much warmer than outside, what type of heat transfer has taken place? 10. In some home heating systems, warm air is blown by a furnace fan into one side of a room. On the other side of the room cold air sinks to the floor. What type of heat transfer is this? 24 Atmosphere

3 Reinforcement Air Movement Directions: Write the term that matches each description below in the spaces provided. Unscramble the letters in the boxes to write a phrase related to the lesson. Use your textbook as a reference. 1. Caused by the uneven heating of Earth and its atmosphere 2. Imaginary line around the middle of Earth 3. Windless zone at the equator which sailing vessels try to avoid 4. Winds generally responsible for the movement of weather across the United States and Canada 5. Winds that provide a dependable route for trade 6. Cool breezes during the day caused by differences in heating and cooling rates of land and water 7. Narrow belts of strong winds at high altitudes which blow near the top of the troposphere 8. Cool breezes at night caused by differences in heating and cooling rates of land and water 9. Heat from the Sun 10. The deflection of air masses resulting from Earth s eastward rotation 11. Winds that blow from the North and South Poles 12. The phrase is: Atmosphere 25

3 Enrichment Thermals Convection is responsible not only for major wind systems that affect the entire Earth but also for small-scale air movements that affect only a small part of Earth s surface. Land and sea breezes are an example of small-scale air movements, or local winds. These small-scale movements are the result of differences in temperature over land and sea. Small Scale Movement Thermals are another type of small-scale movement. Thermals develop over only a few hundred square meters of land and last less than an hour. The formation of thermals is illustrated in the pictures below. Figure 1 shows the thermal beginning as a rising column of air at Earth s surface. In Figure 2, a cap develops at the top. Eventually, the cap breaks off and increases in size as it continues to be forced upward (Figures 3 and 4). At higher altitudes, the thermal develops a donut shape before it dissipates in the cooler air (Figure 5). Thermals may develop where Earth s surface is warm and the overlying air is cool. This may occur anywhere on Earth. The amount of heating at the surface varies, depending upon the amount of solar radiation absorbed by that part of Earth s surface. Figure 1 Figure 2 Figure 3 Figure 4 Figure 5 1. Thermals occur as a result of hot and cold air movements: air rises and air sinks. 2. What eventually causes a thermal to dissipate? 3. Vultures and hawks sometimes glide the thermals. What do you think this means? Why do you think they do it? 28 Atmosphere

Chapter Review Atmosphere Part A. Vocabulary Review Directions: Complete the following sentences using the correct terms. 1. The lowest layer of the atmosphere is the ; it contains clouds and smog. 2. An oxygen form present in the filters ultraviolet radiation from the sun. 3. Heat transfer that occurs when molecules come in contact with one another is. 4. Winds blowing from the northeast to the southwest near the North Pole are known as. 5. Air masses moving in the northern hemisphere are turned westward from their original paths in the. 6. A windless zone at Earth s equator where air rises almost straight up is called the. 7. The reflects radio waves at night. 8. Cool, dense air near the sea moves inland toward warm, dense areas during the day and sets up. 9. At 30 north or south of the equator, air descending to Earth s surface creates steady. 10. The transfer of energy in the form of rays or waves is known as. 11. The blow from southwest to northeast at 30 to 60 latitude in the northern hemisphere. 12. Cool, dense air moves during the night from the land toward water as. 13. Skin cancer can be caused by too much exposure to. 14. Each hemisphere has two narrow belts of fast-moving winds called. Assessment 15. Some chemicals that are being blamed for the destruction of the ozone layer are. Atmosphere 33

Chapter Review (continued) Part B. Concept Review Directions: Describe each of the following concepts on the lines provided. 1. three things that can happen to the energy Earth receives from the Sun 2. the danger of ultraviolet radiation 3. the relationship of radiation, conduction, and convection 4. the destruction of ozone by chlorofluorocarbons 5. the cause of the difference in temperature between the equator and the poles Assessment 6. the two most abundant gases in our atmosphere 7. the factors that affect air pressure 8. the Coriolis effect on wind patterns 9. sea breezes during the day and land breezes at night 34 Atmosphere