Chapter 17 Chapter Review

Slides:



Advertisements
Similar presentations
The Atmosphere.
Advertisements

Chapter 17 Study Guide Answers
Chapter 26 The Atmosphere, Energy in Processes, Insolation, Specific Heat, & Isotherms BFRB Topic 5 & Topic 6.
Handout (yellow) Solar Energy and the Atmosphere Standard 3 Objective 1 Indicators a, b, and c Standard 3 Objectives 1, 2, and 3 Workbook Pages 3,
Chapter 17 Chapter Review Place these notes into your notebook.
Objectives Explain how radiant energy reaches Earth.
17 Atmosphere 17.1 The Atmosphere in Balance
Atmosphere Test Review
Meteorology Vocabulary. 1. Relative Humidity: The % of water vapor the air is holding compared to how much it can hold.Relative Humidity 2. Water Vapor:
Atmospheric Basics Section 11.1 Section Atmospheric Composition Energy is transferred throughout Earth’s atmosphere Energy is transferred throughout.
Chapter 1 Vocabulary Atmosphere Altitude Density Cycle Radiation Conduction Convection Ultraviolet Radiation Infrared Radiation Ozone Greenhouse Effect.
The Dynamic EarthSection 2 Objective #9 Describe the layers of the Earth’s atmosphere.
Atmospheric Heating Radiation Conduction Convection.
Section 3.2 The Atmosphere
Meteorology Chapter 17. Chapter 17.1 While you read 1.Volcanic eruptions  lowered temperature 2.Volcanic eruptions  released gases to form atmosphere.
CHAPTER ONE- SECTION 1- THE AIR AROUND YOU. Key Concepts: 1. What is the composition of Earth’s Atmosphere? 2. How is the atmosphere important to living.
Chapter 17 Study Guide Answers
Weather and Climate The Atmosphere
Section 2: The Atmosphere
Guided Notes about the Earth’s Atmosphere
Unit 9 Section 2: Solar Energy and the Atmosphere
Energy Transfer in the Atmosphere
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Greenhouse Effect How we stay warm.
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Objectives Describe the composition of Earth’s atmosphere.
Greenhouse Effect How we stay warm.
Greenhouse Effect How we stay warm.
Chapter 3 notes Section 2.
Chapter 15: Atmosphere Section 15.1: Earth's Atmosphere
Lesson 1-6.
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Solar Energy Chapter 22.2.
Section 1: Atmospheric Basics
Earth’s Changing Atmosphere
Solar Energy and the Atmosphere
Section 2: The Atmosphere
The Atmosphere Weather and Climate
Section 2: The Atmosphere
Section 2: The Atmosphere
Earth’s Changing Atmosphere
ATMOSPHERE.
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
The Atmosphere and Weather
Section 2: Solar Energy and the Atmosphere
The Dynamic Earth The Atmosphere.
Section 2: The Atmosphere
Seasons and Atmosphere
Section 2 Atmospheric Heating.
The Atmosphere Atmosphere Composition - 76% Nitrogen - 23% Oxygen
“Energy in Earth Processes”
Heating the Atmosphere
Section 2: The Atmosphere
Science 7 Chapter 16 Review and Retake.
Seasons and Atmosphere
Section 2: The Atmosphere
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Section 2: The Atmosphere
Section 2: The Atmosphere
15.3 energy in the atmosphere
Chapter 15 Atmosphere.
Section 2: The Atmosphere
Place these answers onto your Meteorology Chapter 17 Worksheets.
Section 2: The Atmosphere
Place these notes into your Meteorology notebook.
Section 2: The Atmosphere
Section 2: The Atmosphere
Temperature: Factors in Heating
Section 2: The Atmosphere
Chapter 3 Section 2.
Presentation transcript:

Chapter 17 Chapter Review Place these notes into your notebook.

Vocabulary Review conduction, convection Conduction is the transfer of energy through collisions. Convection is the transfer of energy through currents.

Vocabulary Review convection, radiation Convection can transfer energy only within a liquid or gas; it does not require a medium.

Vocabulary Review troposphere, stratosphere Troposphere; lowest layer of atmosphere, temperature decreases with altitude; stratosphere; above troposphere, temperature increases with altitude.

Vocabulary Review The bottom layer in a(n) ___________ of air is colder than the air above it. Temperature inversion

Vocabulary Review On a map, all of the points on a(n)_____________ are the same temperature. isotherm

Vocabulary Review Although in the stratosphere it is beneficial to humans, _____________ near Earth’s surface is harmful to humans. ozone

Concept Review Which gas makes up the most of the atmosphere? nitrogen

Concept Review Describe several ways in which gases enter and exit the atmosphere? Plants remove carbon dioxide from and add oxygen to the air during photosynthesis. Animals remove oxygen from the air when they inhale and add carbon dioxide when they exhale. CO2 is also released as matter decomposes. Water vapor enters the atmosphere through animal exhalations and leaves through precipitation.

Concept Review Why is air warmer at the top of the stratosphere than at the top of the troposphere? Ozone near the top of the stratosphere absorbs ultraviolet rays from the sun.

Concept Review Describe three ways energy is transferred from Earth’s surface to the atmosphere. Radiation transfers energy through space in the form of electromagnetic waves. Conduction transfers energy through collisions of atoms or molecules. Convection transfers energy through currents caused by differences in density in a fluid.

Concept Review If there were no greenhouse gases in the atmosphere, how would Earth’s temperature be different than it is today? Explain your thinking. Earth would be colder because more of the heat radiated by its surface would escape directly into space.

Concept Review Why are the poles colder than the equator? The angle of insolation is less at the poles than at the equator.

Concept Review Describe at least two ways humans increase the amount of carbon dioxide in the atmosphere. The burning of fossil fuels releases carbon dioxide into the air. Deforestation reduces the number of trees available to remove carbon dioxide from the air.

Concept Review Intensity of Insolation 14. Copy and complete the table below to summarize how insolation depends on location and time. Intensity of Insolation   Greatest Least Time of Day around noon nighttime Time of Year summer winter Latitude near equator near poles

Interpreting Graphs 21. In which container did the material warm faster? Container A

Interpreting Graphs In which container did the material cool faster? Container A

Interpreting Graphs 23. Which container held the water? Container B, water absorbs heat more slowly than soil.

Interpreting Graphs 24. Did the soil and water both warm the same amount? Why or why not? No; water needs more energy than does soil to raise its temperature the same amount.

Interpreting Graphs 25. The smallest daily temperature ranges at Earth’s surface are less than 1°C. Where are they and why? What sort of location would usually have the largest temperature range? Why? Over oceans because they heat up and cool down more slowly than land; In a city or in a desert, because sand and building