Directed Reading. Section: Solar Energy and the Atmosphere RADIATION. identical point on the next wave. waves

Similar documents
ATMOSPHERE PACKET CHAPTER 22 PAGES Section 1 page 546

COMPOSITION OF THE ATMOSPHERE

In the space provided, write the letter of the description that best matches the term or phrase. as waves. thermosphere

The Atmosphere - Chapter Characteristics of the Atmosphere

The Atmosphere. Characteristics of the Atmosphere. Section 23.1 Objectives. Chapter 23. Chapter 23 Modern Earth Science. Section 1

Key Concept Heat in Earth s atmosphere is transferred by radiation, conduction, and convection.

Meteorology Pretest on Chapter 2

Unit 3 Review Guide: Atmosphere

Section 2: The Atmosphere

Planetary Atmospheres: Earth and the Other Terrestrial Worlds Pearson Education, Inc.

Chapter 10 Planetary Atmospheres: Earth and the Other Terrestrial Worlds Pearson Education, Inc.

Common Elements: Nitrogen, 78%

2/22/ Atmospheric Characteristics

Chapter 2. Heating Earth's Surface & Atmosphere

Prentice Hall EARTH SCIENCE. Tarbuck Lutgens

Troposphere and mesosphere Stratosphere and thermosphere radio

Chapter 3. Multiple Choice Questions

Lecture Outlines PowerPoint. Chapter 16 Earth Science 11e Tarbuck/Lutgens

The Atmosphere and Atmospheric Energy Chapter 3 and 4

Chapter 9 Atmosphere Study Guide

Chapter 10 Planetary Atmospheres Earth and the Other Terrestrial Worlds. What is an atmosphere? Planetary Atmospheres

1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely

General Comments about the Atmospheres of Terrestrial Planets

The Atmosphere. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left.

Outline. Planetary Atmospheres. General Comments about the Atmospheres of Terrestrial Planets. General Comments, continued

Final Review Meteorology

Science Chapter 13,14,15

Chapter 10 Planetary Atmospheres: Earth and the Other Terrestrial Worlds. What is an atmosphere? About 10 km thick

Overview Atmosphere. Meeting Individual Needs. Directed Reading for Content Mastery

Earth s Atmosphere. Energy Transfer in the Atmosphere. 3. All the energy from the Sun reaches Earth s surface.

Unit 2 Meteorology Test **Please do not write on this test** 5. El Nino & La Nina 6. Photosynthesis 7. Coriolis Effect 8.

Wednesday, September 8, 2010 Infrared Trapping the Greenhouse Effect

ATM S 111: Global Warming Solar Radiation. Jennifer Fletcher Day 2: June

Energy: Warming the earth and Atmosphere. air temperature. Overview of the Earth s Atmosphere 9/10/2012. Composition. Chapter 3.

A) usually less B) dark colored and rough D) light colored with a smooth surface A) transparency of the atmosphere D) rough, black surface

The Atmosphere: Structure and Temperature

CLIMATE AND CLIMATE CHANGE MIDTERM EXAM ATM S 211 FEB 9TH 2012 V1

Let s Think for a Second

Topic 5 Practice Test

Lecture 3: Global Energy Cycle

1. CLIMATOLOGY: 2. ATMOSPHERIC CHEMISTRY:

Space Atmospheric Gases. the two most common gases; found throughout all the layers a form of oxygen found in the stratosphere

3. Which color of the visible light has the shortest wavelength? A) violet B) green C) yellow D) red

Chapter 10 Planetary Atmospheres Earth and the Other Terrestrial Worlds

Chapter 11 Lecture Outline. Heating the Atmosphere

HEATING THE ATMOSPHERE

The Atmosphere. Composition of the Atmosphere. Section 2

Chapter 10 Planetary Atmospheres: Earth and the Other Terrestrial Worlds. What is an atmosphere? Earth s Atmosphere. Atmospheric Pressure

Chapter 10 Planetary Atmospheres: Earth and the Other Terrestrial Worlds

11/18/2010. Only part of the spectrum we can see. A rainbow of colors, each corresponding to a different wavelength.

Lecture 2: Global Energy Cycle

Ch22&23 Test. Multiple Choice Identify the choice that best completes the statement or answers the question.

Lesson Overview. Climate. Lesson Overview. 4.1 Climate

Chapter 10 Planetary Atmospheres Earth and the Other Terrestrial Worlds

WEATHER. Review Note Cards

The Cosmic Perspective Planetary Atmospheres: Earth and the Other Terrestrial Worlds

What Is Air Temperature?

Website Lecture 3 The Physical Environment Part 1

Chapter 4 Lesson 1: Describing Earth s Atmosphere

Name Team Period. Station #1 (drawing)

Temperature Scales

Assessment Schedule 2017 Earth and Space Science: Demonstrate understanding of processes in the atmosphere system (91414)

Chapter 02 Energy and Matter in the Atmosphere

ATS150 Global Climate Change Spring 2019 Candidate Questions for Exam #1

Table of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement

Clouds and Rain Unit (3 pts)

I T A T I O N H B I T B T V A O C J K M R S A T M O S P H E R E

The main components of Earth that affects weather are: 1)

Surface Processes and the Hydrosphere Unit Heating the Earth s Atmosphere Chapter 11 (pg )

EARTH'S ATMOSPHERE. 1. The graph below shows the average concentration of ozone in Earth's atmosphere over Arizona during 4 months of the year.

Fluid Circulation Review. Vocabulary. - Dark colored surfaces absorb more energy.

Physical Geography 1st Exam

IV. Atmospheric Science Section

The inputs and outputs of energy within the earth-atmosphere system that determines the net energy available for surface processes is the Energy

Introduction to Electromagnetic Radiation and Radiative Transfer

The Atmosphere of Earth

MIDTERM REVIEW QUESTIONS - PACKET #2 (75 MULTIPLE CHOICE QUESTIONS)

10.1 TEMPERATURE, THERMAL ENERGY AND HEAT Name: Date: Block: (Reference: pp of BC Science 10)

1 A 3 C 2 B 4 D. 5. During which month does the minimum duration of insolation occur in New York State? 1 February 3 September 2 July 4 December

Lecture 2: Global Energy Cycle

Solar Flux and Flux Density. Lecture 2: Global Energy Cycle. Solar Energy Incident On the Earth. Solar Flux Density Reaching Earth

UNIT TEST PRACTICE TEST

Energy and Insolation Review 2

Which Earth latitude receives the greatest intensity of insolation when Earth is at the position shown in the diagram? A) 0 B) 23 N C) 55 N D) 90 N

G109 Alternate Midterm Exam October, 2004 Instructor: Dr C.M. Brown

C) wavelength C) eastern horizon B) the angle of insolation is high B) increases, only D) thermosphere D) receive low-angle insolation

Earth s Atmosphere About 10 km thick

The order of the atmosphere layers. Unique characteristics of each layer. What do the temperatures do in each layer? Why is the temperature of the

9/1/14. Chapter 2: Heating Earth s Surface and Atmosphere. The Atmosphere: An Introduction to Meteorology, 12 th. Lutgens Tarbuck

The Layered Atmosphere:

4-1 The Role of Climate

1 Characteristics of the Atmosphere

4-1 The Role of Climate

Earth s Atmosphere. Composition

Atmosphere. Transfer in the Atmosphere

Energy Transfer Packet 9

Period 13 Solutions: Earth as an Energy System

Energy Balance and Temperature. Ch. 3: Energy Balance. Ch. 3: Temperature. Controls of Temperature

Energy Balance and Temperature

ATMOSPHERIC ENERGY and GLOBAL TEMPERATURES. Physical Geography (Geog. 300) Prof. Hugh Howard American River College

Transcription:

Skills Worksheet Directed Reading Section: Solar Energy and the Atmosphere 1. How is Earth s atmosphere heated? 2. Name the two primary sources of heat in the atmosphere. RADIATION In the space provided, write the letter of the description that best matches the term or phrase. 3. radiation 4. wavelength 5. electromagnetic waves 6. electromagnetic spectrum a. the waves that make up all forms of radiation b. the distance from any point on a wave to the identical point on the next wave c. all of the frequencies or wavelengths of electromagnetic radiation d. all forms of energy that travel through space as waves, including the energy that Earth receives from the sun 7. What form of radiation can humans see? 8. What are three forms of radiation that humans cannot see? 9. How fast do waves of radiation travel through space? 10. How are the wavelengths of visible light seen? Holt Earth Science 15 The Atmosphere

11. Which wavelengths are shorter than visible light? Which are longer? THE ATMOSPHERE AND SOLAR RADIATION 12. Almost all radiation that has a wavelength shorter than the wavelengths of visible light is absorbed by the a. lower atmosphere. b. thermosphere. c. upper atmosphere. d. stratosphere. 13. X rays, gamma rays, and ultraviolet rays are absorbed by molecules of nitrogen and oxygen in the mesosphere and a. lower atmosphere. b. thermosphere. c. upper atmosphere. d. stratosphere. 14. Ultraviolet rays are absorbed and act upon oxygen molecules to form ozone in the a. lower atmosphere. b. thermosphere. c. upper atmosphere. d. stratosphere. 15. Solar rays with longer wavelengths, such as visible and infrared waves, reach the a. lower atmosphere. b. thermosphere. c. upper atmosphere. d. stratosphere. 16. Most incoming infrared radiation is absorbed by carbon dioxide, water vapor, and other complex molecules in the. Holt Earth Science 16 The Atmosphere

17. How much of the radiation from visible light waves is absorbed as they pass through the atmosphere? 18. What causes scattering? 19. What happens when particles and gas molecules in the atmosphere reflect and bend solar rays? 20. What does scattering do to solar rays that are traveling to Earth? 21. What effect does scattering have on the sky s appearance? 22. What happens to solar energy that reaches Earth s surface? Holt Earth Science 17 The Atmosphere

23. What are eight characteristics on which the amount of energy that is absorbed or reflected by Earth s surface depends? 24. What is the fraction of solar radiation that is reflected off a particular surface called? 25. What is Earth s albedo? Explain your answer. ABSORPTION AND INFRARED ENERGY 26. Solar radiation that is not reflected is a. absorbed. b. scattered. c. radiated. d. dissipated. 27. When Earth s surface absorbs solar radiation, the surface materials are heated by a. longer-wavelength infrared rays and ultraviolet light. b. short-wavelength infrared rays and visible light. c. short-wavelength microwaves and infrared light. d. longer-wavelength microwaves and ultraviolet light. Holt Earth Science 18 The Atmosphere

28. Heated materials on Earth s surface convert energy into infrared rays of longer wavelengths and a. reabsorb energy as infrared waves. b. reabsorb energy as radio waves. c. reemit energy as infrared rays. d. reemit energy as radio waves. 29. What happens to the infrared rays that are reemitted into the atmosphere? 30. What does the absorption of thermal energy from the ground do to Earth s surface? 31. Warm air near Earth s surface sometimes bends light rays to cause an effect called a. 32. One process that helps heat Earth s atmosphere that is similar to the process that heats a greenhouse is called the. 33. The warming of the surface and lower atmosphere of Earth that occurs when carbon dioxide, water vapor, and other gases in the air absorb and reradiate infrared radiation is called the. 34. How does the amount of solar energy that enters Earth s atmosphere generally compare to the amount that escapes into space? 35. What is one human activity that may have caused the average temperature of the atmosphere to increase in recent years? Holt Earth Science 19 The Atmosphere

VARIATIONS IN TEMPERATURE 36. What is the primary factor that affects how much solar energy reaches any point on Earth s surface? a. surface features b. time of year c. latitude d. time of day 37. Near the equator, the rays of the sun strike the ground at an angle of about a. 90%. b. 45%. c. 60%. d. 10%. 38. Temperatures are higher at the equator because a. solar energy is spread out over a larger area. b. solar energy is concentrated in a small area. c. clouds hold in the solar energy. d. more solar energy is reflected into space. 39. Seasonal variations in temperature occur because of a. the changing distance between Earth and the sun. b. the speed of Earth s rotation. c. the tilt of Earth s axis. d. the variations in the sun s energy. 40. Why does the amount of water in the air affect the temperature of a region? a. Water vapor reflects sunlight. b. Water vapor cools the air. c. Water vapor creates clouds. d. Water vapor stores heat. 41. Which regions will generally have more moderate temperatures? a. regions in which winds blow from the land b. regions receiving ocean winds c. regions receiving high winds d. regions receiving little rain 42. Why are the warmest hours of the day usually mid- to late afternoon? Holt Earth Science 20 The Atmosphere

43. What happens to the energy when sunlight hits Earth at an angle smaller than 90? 44. Why are average temperatures higher at the equator than near the poles? 45. Why does the Northern Hemisphere have higher temperatures for one part of the year and lower temperatures the rest? 46. Why does the amount of water in the air affect the temperature of a region? 47. Why do areas of high elevation become warm during the day and cool quickly at night? 48. Why do desert temperatures vary widely between day and night? 49. Why are land areas close to large bodies of water generally cooler during the day and warmer at night than similar inland areas? Holt Earth Science 21 The Atmosphere

CONDUCTION 50. As they become heated, molecules in a substance a. move at the same rate as when they are cooled. b. move faster. c. move more slowly. d. do not move at all. 51. What effect do collisions between molecules have on the molecules? a. It changes their structure. b. It breaks them apart. c. It cools them. d. It warms them. 52. The transfer of energy as heat from one substance to another by direct contact is called a. conduction. b. collision. c. firing. d. baking. 53. Solid substances are good conductors because a. molecules are close together. b. molecules are far apart. c. molecules cannot collide. d. molecules move slowly. 54. Air is a poor conductor because a. molecules are close together. b. molecules are far apart. c. molecules cannot collide. d. molecules move slowly. 55. Conduction heats only the lowest few centimeters of the atmosphere because a. air does not come into direct contact with Earth. b. air comes into direct contact with Earth. c. molecules of air in the lower atmosphere are closer together. d. molecules in the upper atmosphere do not collide. CONVECTION 56. What is the primary cause of the heating of the lower atmosphere? Holt Earth Science 22 The Atmosphere

57. The movement of matter due to differences in density caused by temperature variations resulting in the transfer of heat is called. 58. When does convection occur? 59. What happens to air heated by radiation or conduction? 60. How is Earth s atmosphere warmed evenly? 61. Why is the atmospheric pressure lower beneath a mass of warm air? 62. Explain how atmospheric pressure differences create winds. Holt Earth Science 23 The Atmosphere