Troposphere and mesosphere Stratosphere and thermosphere radio

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

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

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

Section 2: The Atmosphere

1 Characteristics of the Atmosphere

The Atmosphere - Chapter Characteristics of the Atmosphere

Common Elements: Nitrogen, 78%

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

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

1. CLIMATOLOGY: 2. ATMOSPHERIC CHEMISTRY:

The Atmosphere. Composition of the Atmosphere. Section 2

2/22/ Atmospheric Characteristics

Unit 3 Review Guide: Atmosphere

WATER IN THE ATMOSPHERE

The troposphere is the layer closest to Earth s surface. Extends from 9-16 km above Earth s Surface It contains most of the mass of the atmosphere.

Atmosphere & Heat Transfer Basics Notes

Name Team Period. Station #1 (drawing)

Chapter 4 Lesson 1: Describing Earth s Atmosphere

COMPOSITION OF THE ATMOSPHERE

Wednesday February 1 st, Daily Science: How are the upper and the lower part of the stratosphere different?

Atmospheric Basics Atmospheric Composition

Very Dynamic! Energy in the Earth s Atmosphere. How Does it Get Here? All Objects Radiate Energy!

ATMOSPHERE PACKET CHAPTER 22 PAGES Section 1 page 546

Let s Think for a Second

The Atmosphere EVPP 110 Lecture Fall 2003 Dr. Largen

Science Chapter 13,14,15

General Comments about the Atmospheres of Terrestrial Planets

anemometer a weather instrument that measures wind speed with wind-catching cups (SRB, IG)

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

Energy Transfer Packet 9

The Atmosphere. 1 Global Environments: 2 Global Environments:

The Atmosphere of Earth

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

WEATHER. Review Note Cards

Atmospheric Layers. Ionosphere. Exosphere. Thermosphere. Mesosphere. Stratosphere. Troposphere. mi (km) above sea level 250 (400) 50 (80) 30 (50)

1 Characteristics of the Atmosphere

Evolution of the Atmosphere

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

Earth! Objectives: Interior and plate tectonics Atmosphere and greenhouse effect

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

Energy, Temperature, & Heat. Energy, Temperature, & Heat. Temperature Scales 1/17/11

Final Review Meteorology

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

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

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

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

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

Goal 2.5. The Atmosphere

Composition, Structure and Energy. ATS 351 Lecture 2 September 14, 2009

Warm Up 1: Atmosphere LT I can describe dew point, condensation nuclei and explain the difference between relative and absolute humidity.

Atmosphere. Transfer in the Atmosphere

NAME BLOCK WEATHER STUDENT PACKET WEATHER WARM UPS WEATHER VOCABULARY ATMOSPHERE GASES CAREERS

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

The Atmosphere and Atmospheric Energy Chapter 3 and 4

Prentice Hall EARTH SCIENCE. Tarbuck Lutgens

Final Weather Unit Study Guide

The Atmosphere. Importance of our. 4 Layers of the Atmosphere. Introduction to atmosphere, weather, and climate. What makes up the atmosphere?

Our Atmosphere as seen from the bottom of it near Grand Pre, NS. Info modified from various sources by TWebb HHS

Heating the Atmosphere (Chapter 14, with material from Chapter 2)

Atmosphere L AY E RS O F T H E AT MOSPHERE

Meteorology Pretest on Chapter 2

Chapter 9 Atmosphere Study Guide

A Quick Look at the Atmosphere and Climate

Energy Transfer in the Atmosphere

The Atmosphere. Topic 3: Global Cycles and Physical Systems. Topic 3: Global Cycles and Physical Systems. Topic 3: Global Cycles and Physical Systems

* Defining Temperature * Temperature is proportional to the kinetic energy of atoms and molecules. * Temperature * Internal energy

Earth s Atmosphere About 10 km thick

Chapter 2. Heating Earth's Surface & Atmosphere

Answer the following questions. Answers that cannot be read will be counted as incorrect. 1. What is weather? 2. What is Earth s atmosphere?

AST 105 Intro Astronomy The Solar System

2. What does a mercury barometer measure? Describe this device and explain how it physically works.

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

78% : component of atmosphere! 21% : 1% : Changes depending on origin of air: - originated over - originated over Ozone = O 3 Definition:

Global Energy Balance: Greenhouse Effect

FCAT Review Earths Systems

Lecture 4: Global Energy Balance

Lecture 4: Global Energy Balance. Global Energy Balance. Solar Flux and Flux Density. Blackbody Radiation Layer Model.

Mr. Lanik Practice Test Name:

Energy and Insolation Review 2

Heat Transfer. Conduction, Convection, and Radiation. Review: Temperature

Atmosphere.notebook January 03, 2013

surrounds Earth and protects it somewhat from solar radiation. Like all other matter, air has weight,

Radiation and the atmosphere

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

Thermal Energy. Chapter 6 2 Transferring Thermal Energy

Planetary Temperatures

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.

Average Temperature Readings at Various Altitudes

Wednesday, September 8, 2010 Infrared Trapping the Greenhouse Effect

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

10/31/2017. Calculating the temperature of earth (The greenhouse effect) IR radiation. The electromagnetic spectrum

Planetary Atmospheres

The of that surrounds the Earth. Atmosphere. A greenhouse that has produced the most global. Carbon Dioxide

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

Website Lecture 3 The Physical Environment Part 1

Now that we know, more or less, what air is made of, let's talk a bit about it's physical properties.

Unit 5. Seasons and Atmosphere

Chapter 15 The Atmosphere and Weather

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

Today. Events. Terrestrial Planet Geology - Earth. Terrestrial Planet Atmospheres. Homework DUE next time

Transcription:

Warm-up Page: 518, 1. What two layers of the atmosphere is temperature decreasing? Troposphere and mesosphere Page: 518, 2. What two layers of the atmsophere is temperature increasing? Stratosphere and thermosphere Page: notes, 3.The ionosphere makes it possible for worldwide communication possible. radio 1

Objective: SWBAT SWBAT describe the three ways that energy is transferred in the atmosphere. Define: greenhouse effect, radiation, conduction, convection Explain how humans may be contributing to the greenhouse effect 2

Objective: SWBAT 3 rd / 5 th Understand the temp. changes are how atmospheric layers are identified Complete atmosphere layer graph and label correct area based on temperature Place correct location of features based on altitude and temperatures Compare/contrast the layers of the atmosphere Understand that temperature changes or varies with altitude Temperature range and change is how scientist label regions (layers of atmosphere) Understand as altitude increase air pressure decreases Explain why a helium balloon expands when it rises Why does NASA use rockets to study upper atmosphere

Activities: Warm-up & quiz Notes and discussion Review crossword sec. 19.1 4

Energy Transfer in the Atmosphere SEC. 19-2 5

Objectives: S.W.B.A.T. Understand and compare and contrast radiation, convection & conduction Complete heat budget chart of atmosphere Explain why the atmosphere acts like a blanket

Activities: Warm-up Notes and discussion Complete review handout on transfer of energy methods Heat budget & solar radiation handout Upper atmosphere 1-4 H.W.

Energy From the Sun The sun is the source of all energy in our atmosphere Three things happen to the energy received from the sun. 1. - about 30% is reflected back 2. - about 20% is absorbed by the atmosphere 3. - about 50% passes through & absorbed by land and water

Energy Transfer There are three different ways that energy can be transferred from one substance to another 1. Radiation 2. Conduction 3. Convection 9

Radiation The transfer of heat in the form of waves.

Electromagnet radiation forms 11

Radiation: Scattering of Light Clouds, dust, water droplets, and other molecules in the atmosphere disrupt the paths of radiation from the sun and cause scattering. As a result, the sunlight that reaches Earth s surface comes from all directions. The sky appears blue, due to wavelength of blue-light is scattered more by N2 & O2. 12

13

Radiation: Reflection of Light Some of the radiation that reaches Earth is reflected back. Albedo the amount of solar radiation that is reflected off the surface of an object. 14

The Greenhouse Effect Earth s atmosphere slows the escape of energy that radiates from Earth s surface just as the glass in a greenhouse does. Greenhouse effect - 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 radiation Things Heat Up!

The Greenhouse Effect Scientists believe that human behaviors that increase CO2 and H2O vapor add to the greenhouse effect making Earths overall temp. to rise.. 16

Conduction Conduction - the transfer of energy as heat through a material by direct contact. Collisions between the particles result in the transfer of energy, which warms the substance. Has to involve direct contact.(touch)

Conduction The transfer of heat when two objects touch.

19

20

http://www.youtube.com/watch?v =7Y3mfAGVn1c 21

Convection Convection - the movement of fluid(liquid, gas) matter due to differences in density that are caused by temperature variations The continuous cycle in which cold air sinks and warm air rises and spreads energy in Earth s atmosphere.

Convection Warm air (less dense than cool air) exerts less pressure than the same volume of cooler air does. The less dense Warm air is pushed upward

24

25

Convection The transfer of heat through liquids or gasses. - Warm air rising - Cold air sinking

27

Energy in the Atmosphere Heat transfer by convection Heat transfer by convection Heat transfer by radiation Heat transfer by conduction

29

30

Cool down 1. Hot air rising and cool air sinking is a type of heat transfer called: Convection 2. Heat lamp (infrared energy) keeping French fries warm is what type of heat transfer? radiation 31

Cool down 1. As you increase altitude the air pressure does this? What instrument would measure this? Decreases, barometer 2. The special area known as the ionosphere is located in what main layer of the atmosphere? thermosphere 32