The Coriolis Effect - Deflect the Arrows!

Size: px
Start display at page:

Download "The Coriolis Effect - Deflect the Arrows!"

Transcription

1 NAME: DATE: The Coriolis Effect - Deflect the Arrows Directions: The Circle below represents the Earth. The equator is present, dividing the image into the Northern and Southern hemispheres. The arrows represent wind direction. 1. Using a DASHED LINE, correctly deflect each arrow as the wind would naturally be deflected. HINT: Look DOWN the arrow towards the point, even if that means turning your paper around.deflect (curve) to the RIGHT in the Northern Hemisphere and to the LEFT in the Southern Hemisphere. North Pole South Pole equator

2 Answer all questions on this page. If you need help, you can visit this site for a short summary about the Coriolis Effect: Infoplease Encyclopedia: Coriolis Effect. 1- What is the Coriolis Effect? 2- What causes the Coriolis Effect? 3- Name 3 things affected by the Coriolis Effect 4- What do you think a soldier firing a missile or a pilot flying a plane must do in order to accurately land the missile or the plane at the correct destination?

3 1.Using the picture above, please draw, label, and indicate the direction of air as seen by an earthling for the following: 1. An arrow showing which way the Earth rotates. 2.The four Hadley cells, four Ferrel cells, four Polar cells. 3.The Westerlies 4.The Tradewinds

4 Do the following activity. You will need to work with a partner. Materials You will two balloons and two markers (different colors) Procedure 1. Blow up a balloon. 2. With a marker, draw the equator on the balloon and label the North and South Poles. 3. Hold the balloon at eye level and rotate it left to right, simulating the rotation of the earth. 4. While one partner rotates the earth balloon, the other examines the movement of the earth from the North Pole perspective and from the South Pole perspective. 5. While one partner continues to rotate the balloon steadily from left to right, the other slowly tries to draw a line straight south from the North Pole to the equator. Using the other marker and while the earth continues to rotate, draw a line straight north from the South Pole to the equator. 6. Do the experiment again but switch roles. Conclusion Answer questions 1-5 below. 1. As you look down from the North Pole toward the equator, which way is the balloon spinning, clockwise or counterclockwise? 2. As you look up from the South Pole toward the equator, which way is the balloon spinning, clockwise or counterclockwise? 3. What happened when you tried to draw a straight line from the North Pole to the equator? 4. What happened when you tried to draw a straight line from the South Pole to the equator?

5 5. Predict what would happen if you again drew lines in the Northern and Southern Hemispheres but with the earth rotating in the opposite direction. Fill in the blanks below 1. Warm air, expands and cools. Then it sinks downward to where the rising warm air was located. This thermal cycle of moving air is called a current. Unequal heating of Earth s surface causes air circulation: air at the equator gets more energy from the Sun, and the heated air rises and moves toward the regions. Here it cools in the upper atmosphere, sinks towards the, and is drawn back to the warmer regions of the equator. 2. Since the Earth on its axis, the pathway of the moving air is affected. All free- moving objects, including air and water, aircraft and missiles, appear to deviate from their straight-line paths. This apparent shift due to Earth s rotation is called the. 3. The Coriolis effect deflects winds toward the in the Northern Hemisphere and toward the left in the Hemisphere. The faster the wind, the greater the deflection. This deflection causes global wind patterns. At the equator the atmospheric circulation is referred to as cells. On the surface of the Earth the global wind pattern is called the winds. Between 30 and 60 degrees north and south latitude the atmospheric circulation is referred to as cells. On

6 the surface of the Earth the global wind pattern is called the. Answer the question below to summarize the Coriolis Effect 1. In the Northern Hemisphere, free-moving objects traveling over large distances are deflected to the of their intended path of motion. are deflected to the of their intended path of motion. 3. If a missile is launched from the North Pole, toward an object on the equator, should it be aimed to the left, to the right, or directly at its target? EXPLAIN YOUR ANSWER. 2. In the Southern Hemisphere, free-moving objects traveling over large distances 4. If a missile is launched from the equator toward an object in the Northern Hemisphere, should it be aimed to the left, to the right, or directly at its target? EXPLAIN YOUR ANSWER. 5. A flight from Salt Lake City, CT to New York, NY takes about 6 hours. The return trip takes about 5 hours. Why does this happen?

Wind and Air Pressure

Wind and Air Pressure Wind and Air Pressure When air moves above the surface of the Earth, it is called wind. Wind is caused by differences in air pressure. When a difference in pressure exists, the air will move from areas

More information

Wind Movement and Global and Local Winds

Wind Movement and Global and Local Winds Wind Movement and Global and Local Winds In previous lessons, you learned that the uneven heating of Earth s surface by the Sun causes some areas to be warmer than others. This uneven heating of land forms

More information

Copy and answer the following in your marble composition book. 1. Which direction is the wind deflected in the northern hemisphere?

Copy and answer the following in your marble composition book. 1. Which direction is the wind deflected in the northern hemisphere? Copy and answer the following in your marble composition book. 1. Which direction is the wind deflected in the northern hemisphere? 2. Which direction is the wind deflected in the southern hemisphere?

More information

3 Global Winds and Local Winds

3 Global Winds and Local Winds CHAPTER 15 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?

More information

3 Global Winds and Local Winds

3 Global Winds and Local Winds CHAPTER 6 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?

More information

Think it Over. Now that we have completed the activity, make any necessary changes to your prediction.

Think it Over. Now that we have completed the activity, make any necessary changes to your prediction. Think it Over What do global wind patterns look like? Draw your prediction on your sheet. Now, let s try something. Does the wind turn? Let s find out! Now that we have completed the activity, make any

More information

Global Winds and Local Winds

Global Winds and Local Winds Global Winds and Local Winds National Science Education Standards ES 1j What is the Coriolis effect? What are the major global wind systems on Earth? What Causes Wind? Wind is moving air caused by differences

More information

ATMOSPHERIC CIRCULATION

ATMOSPHERIC CIRCULATION Name ATMOSPHERIC CIRCULATION (adapted from Dr. S. Postawko, U. of Ok.) INTRODUCTION Why does the wind blow? Why do weather systems in the mid-latitudes typically move from west to east? Now that we've

More information

Carolina TM Coriolis Effect and Atmospheric Circulation Kit STUDENT GUIDE

Carolina TM Coriolis Effect and Atmospheric Circulation Kit STUDENT GUIDE Name: Date: Mods: Carolina TM Coriolis Effect and Atmospheric Circulation Kit STUDENT GUIDE Background Global air circulation is a major influence on the world's climates. Air circulation is caused by

More information

Finish Characteristics of Climate

Finish Characteristics of Climate Bell Ringer Finish Characteristics of Climate Wind Coriolis Effect Newton s second law: a body in motion will continue in motion (unchanged) unless acted upon by an outside force. Liquid (water) and gas

More information

ATOMOSPERIC PRESSURE, WIND & CIRCULATION

ATOMOSPERIC PRESSURE, WIND & CIRCULATION ATOMOSPERIC PRESSURE, WIND & CIRCULATION A. INTRODUCTION Important because: pressure patterns drive wind patterns which in turn drive oceanic circulation patterns o atmospheric & oceanic circulation: major

More information

Full Name: Class: Period: Date:

Full Name: Class: Period: Date: Topic/Objective: Essential Question: Full Name: Class: Period: Date: Tutor Use Only: Air Pressure and Wind (Chapter 19) Air Pressure the weight of the atmosphere pushing down on the Earth exerting a force

More information

Lecture The Oceans

Lecture The Oceans Lecture 22 -- The Oceans ATMOSPHERE CIRCULATION AND WINDS Coriolis effect Prevailing winds and vertical circulation Zones of pressure, evap. & ppt. Factors modifying global winds -- Differential heating

More information

6.1 Introduction to Weather Weather air mass Weather factors Temperature Pressure What is wind? Wind Convection in the atmosphere Thermals thermal

6.1 Introduction to Weather Weather air mass Weather factors Temperature Pressure What is wind? Wind Convection in the atmosphere Thermals thermal 6.1 Introduction to Weather Weather is a term that describes the condition of the atmosphere in terms of temperature, atmospheric pressure, wind, and water. The major energy source for weather events is

More information

Trade winds Prevailing westerlies east

Trade winds Prevailing westerlies east Warm-up Page: 528, 1. What is the major wind belt that is nearest the equator? Trade winds Page: 528, 2. What is the major wind belt that the most of the USA belongs to: Prevailing westerlies Page: 528,

More information

EARTH SCIENCE 5.9 (WIND) WEATHER

EARTH SCIENCE 5.9 (WIND) WEATHER EARTH SCIENCE 5.9 (WIND) WEATHER Video Notes Key Points: 1. According to the video, what two factors cause wind: a. b. 2. Fill in the blanks from this quote from the video: Energy from the Sun heats the,

More information

3 Global Winds and Local Winds

3 Global Winds and Local Winds CHAPTER 1 3 Global Winds and Local Winds SECTION The Atmosphere BEFORE YOU READ After you read this section, you should be able to answer these questions: What causes wind? What is the Coriolis effect?

More information

Atmospheric Circulation

Atmospheric Circulation Atmospheric Circulation Why do we say Earth's temperature is moderate? It may not look like it, but various processes work to moderate Earth's temperature across the latitudes. Atmospheric circulation

More information

T. James Noyes, El Camino College Winds Unit (Topic 8A-1) page 1

T. James Noyes, El Camino College Winds Unit (Topic 8A-1) page 1 T. James Noyes, El Camino College Winds Unit (Topic 8A-1) page 1 Name: Section: Winds Unit (3 pts) The Ocean and the Atmosphere We need to learn about the atmosphere, because the ocean and atmosphere are

More information

Lesson: Atmospheric Dynamics

Lesson: Atmospheric Dynamics Lesson: Atmospheric Dynamics By Keith Meldahl Corresponding to Chapter 8: Atmospheric Circulation Our atmosphere moves (circulates) because of uneven solar heating of the earth s surface, combined with

More information

Earth s Atmosphere. Air Currents

Earth s Atmosphere. Air Currents CHAPTER 12 Earth s Atmosphere LESSON 3 Air Currents What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with

More information

What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of

What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of What is Wind? Winds are caused by differences in air pressure. This is horizontal movement of air of high pressure to low pressure. Unequal heating of the atmosphere. Measuring Wind Wind direction is determined

More information

Section 1. Global Wind Patterns and Weather. What Do You See? Think About It. Investigate. Learning Outcomes

Section 1. Global Wind Patterns and Weather. What Do You See? Think About It. Investigate. Learning Outcomes Chapter 5 Winds, Oceans, Weather, and Climate Section 1 Global Wind Patterns and Weather What Do You See? Learning Outcomes In this section, you will Determine the effects of Earth s rotation and the uneven

More information

Chapter: Atmosphere Section 3: Air Movement

Chapter: Atmosphere Section 3: Air Movement Table of Contents Chapter: Atmosphere Section 3: Air Movement We will learn about Air Movement=Wind -Why different latitudes on Earth will receive different amounts of Solar Energy -The Coriolis Effect

More information

Wind in the Atmosphere

Wind in the Atmosphere Lesson 2 Wind in the Atmosphere ESSENTIAL QUESTION What is wind? By the end of this lesson, you should be able to explain how energy provided by the sun causes atmospheric movement, called wind. p 6.ESS2.2,

More information

Warm-up. color mass. albedo. mirage

Warm-up. color mass. albedo. mirage Warm-up Page: 523, 1. The amount of solar energy reflected or absorbed depends on the, texture, composition, volume,, transparency and other properties. color mass Page: 523, 2. The fraction of solar radiation

More information

Read each slide, some slides have information to record on your organizer. Some slides have numbers that go with the question or red and underlined

Read each slide, some slides have information to record on your organizer. Some slides have numbers that go with the question or red and underlined Read each slide, some slides have information to record on your organizer. Some slides have numbers that go with the question or red and underlined to use for answering the questions. Essential Question:

More information

Chapter 7 Weather and Climate

Chapter 7 Weather and Climate Chapter 7 Weather and Climate *Describe what weather is, what affects it, and where it occurs. *Explain the connection between air pressure and wind. * *Many factors affect a region s weather. * *atmosphere

More information

Circulation Patterns

Circulation Patterns Nov. 1, 2017 Today Finish Vertical Atmospheric Structure, Origin, Escape Start Atmospheric Circulation (may finish in 2nd lecture, on Friday) A few words of introduction on Pluto Friday 11AM: Student presentations

More information

Section 3: Atmospheric Circulation

Section 3: Atmospheric Circulation Section 3: Atmospheric Circulation Preview Key Ideas The Coriolis Effect Global Winds Local Winds Maps in Action Key Ideas Explain the Coriolis effect. Describe the global patterns of air circulation,

More information

6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of

6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of 6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of elements comprise the largest portion of oceans and atmosphere

More information

Chapter: Atmosphere Section 3: Air Movement

Chapter: Atmosphere Section 3: Air Movement Table of Contents Chapter: Atmosphere Section 3: Air Movement We will learn about: -Air Movement=Wind -Why different latitudes on Earth will receive different amounts of Solar Energy -The Coriolis Effect

More information

Prevailing Winds. The Coriolis Effect

Prevailing Winds. The Coriolis Effect Prevailing Winds 1. Wind: a movement of air in the atmosphere. Bill Nye wind (2 minutes) 2. Local or regional wind: occur in fairly small areas. 3. Prevailing winds: Major wind pattern that affect large

More information

Wind Patterns on Earth

Wind Patterns on Earth Wind Patterns on Earth What causes air to move? Air pressure differences causes air to move. These differences in air pressure at the same altitude is caused by uneven heating of the Earth s surface. With

More information

W3 Global Circulation Systems

W3 Global Circulation Systems W3 Global Circulation Systems Which regions of Earth receive the most energy from the Sun? If not for global circulation systems There would only be two narrow regions that would support life What

More information

SIO20 - Midterm Examination 2 v1 Winter Section A. Circle the letter corresponding to the best answer. (1 point each)

SIO20 - Midterm Examination 2 v1 Winter Section A. Circle the letter corresponding to the best answer. (1 point each) NAME: Section A. Circle the letter corresponding to the best answer. (1 point each) 1. Rainbows result from: a. refraction and reflection of sunlight by water droplets b. reflection of sunlight by oceans

More information

Atmosphere & Weather. Earth Science

Atmosphere & Weather. Earth Science Atmosphere & Weather Earth Science Energy Transfer in the Atmosphere Earth s energy is provided by the SUN! Energy is important to us because it 1. Drives winds and ocean currents. 2. Allows plants to

More information

Wind in the Atmosphere

Wind in the Atmosphere Lesson 1 Wind in the Atmosphere Essential Question What is wind? By the end of this lesson, you should be able to explain how energy provided by the sun causes atmospheric movement, called wind. 8.10A

More information

WINDS Understand the cause of wind and how it affects climate Chapter 4 Pages 59-67

WINDS Understand the cause of wind and how it affects climate Chapter 4 Pages 59-67 WINDS Understand the cause of wind and how it affects climate Chapter 4 Pages 59-67 What is Wind? A wind is a horizontal movement of air across a surface. Vertical movements are currents or updrafts and

More information

Air Pressure and Wind

Air Pressure and Wind Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. Air pressure is exerted in all directions down, up, and sideways. The

More information

Write on your own paper.

Write on your own paper. Catalyst: 1. During the day, which one heats up faster, land or water? WHY?? 2. During the night which one cools down slower? 3. How does heat move? (hint: from what to what?) 4. What are the differences

More information

The Real Atmosphere. The Real Atmosphere. The Real Atmosphere. The Real Atmosphere

The Real Atmosphere. The Real Atmosphere. The Real Atmosphere. The Real Atmosphere Effect of Seasons & Continents Disrupt global continuity of latitudinal belts of high and low pressure Effect of Seasons & Continents Water has a greater heat capacity than land More energy needed to raise

More information

Chapter. Air Pressure and Wind

Chapter. Air Pressure and Wind Chapter Air Pressure and Wind 19.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. 19.1 Understanding Air Pressure Air Pressure Defined Air pressure

More information

SIXTH GRADE OCEANS 1 WEEK LESSON PLANS AND ACTIVITIES

SIXTH GRADE OCEANS 1 WEEK LESSON PLANS AND ACTIVITIES SIXTH GRADE OCEANS 1 WEEK LESSON PLANS AND ACTIVITIES WATER CYCLE OVERVIEW OF SIXTH GRADE WATER WEEK 1. PRE: Evaluating components of the water cycle. LAB: Experimenting with porosity and permeability.

More information

Atmosphere Circulation

Atmosphere Circulation Atmosphere Circulation Winds What Causes Winds? Difference in air pressure due to unequal heating of the atmosphere. Temperatures vary according to the amount of sun it gets. Uneven heating of the Earth

More information

Friday, February 8 th. Winds/Coriolis Worksheet: Due Today Lab Worksheet: Finish Questions

Friday, February 8 th. Winds/Coriolis Worksheet: Due Today Lab Worksheet: Finish Questions Ocean Currents Friday, February 8 th Winds/Coriolis Worksheet: Due Today Lab Worksheet: Finish Questions Non-rotating Earth Convection cell model Add rotation and add landmasses unequal heating and cooling

More information

IN THE TABLE OF CONTENTS AND ON THE NEXT CLEAN PAGE, TITLE IT: WIND NOTES WIND!

IN THE TABLE OF CONTENTS AND ON THE NEXT CLEAN PAGE, TITLE IT: WIND NOTES WIND! IN THE TABLE OF CONTENTS AND ON THE NEXT CLEAN PAGE, TITLE IT: WIND NOTES WIND! Wind 8.10A recognize that the Sun provides the energy that drives convection within the atmosphere and oceans, producing

More information

Satellites, Weather and Climate Activity: Air & water lab Created by: Mike Burris, Champlain Valley Union High School, VT

Satellites, Weather and Climate Activity: Air & water lab Created by: Mike Burris, Champlain Valley Union High School, VT Satellites, Weather and Climate Activity: Air & water lab Created by: Mike Burris, Champlain Valley Union High School, VT Grade Level: 9-10 Social Studies Curriculum Topic Standards: Subject Keywords:

More information

For Class Today How does ocean water circulate? Ocean currents, surface currents, gyres, currents & climate, upwelling, deep ocean circulation

For Class Today How does ocean water circulate? Ocean currents, surface currents, gyres, currents & climate, upwelling, deep ocean circulation For Class Today Modified Cornell Notes on section 16.1 (pg. 448-453) **Follow the guide in your ISN and previous notes for help** Heading: How does ocean water circulate? Left hand side categories: Ocean

More information

Atmospheric Circulation. Recall Vertical Circulation

Atmospheric Circulation. Recall Vertical Circulation Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and Sea Breezes Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation

More information

Air Pressure and Wind. Goal: Explain the formation of wind based on differences in air pressure

Air Pressure and Wind. Goal: Explain the formation of wind based on differences in air pressure Air Pressure and Wind Goal: Explain the formation of wind based on differences in air pressure What is Air Pressure? Reminder: Air pressure is thickest near Earth s surface and becomes thinner as we move

More information

18.1 Understanding Air Pressure 18.1 Understanding Air Pressure Air Pressure Defined Measuring Air Pressure Air pressure barometer

18.1 Understanding Air Pressure 18.1 Understanding Air Pressure Air Pressure Defined Measuring Air Pressure Air pressure barometer 18.1 Understanding Air Pressure 18.1 Understanding Air Pressure Air Pressure Defined Air pressure is the pressure exerted by the weight of air. Air pressure is exerted in all directions down, up, and sideways.

More information

Wednesday, September 27, 2017 Test Monday, about half-way through grading. No D2L Assessment this week, watch for one next week

Wednesday, September 27, 2017 Test Monday, about half-way through grading. No D2L Assessment this week, watch for one next week Wednesday, September 27, 2017 Test Monday, about half-way through grading No D2L Assessment this week, watch for one next week Homework 3 Climate Variability (due Monday, October 9) Quick comment on Coriolis

More information

Local and Global Winds

Local and Global Winds PART 2 Wind Local and Global Winds Wind is the horizontal movement of air. All wind is caused by air pressure differences due to the uneven heating of Earth's surface, which sets convection currents in

More information

Consequences of the Earth's Rotation

Consequences of the Earth's Rotation Consequences of the Earth's Rotation The earth rotates onits axis taking approximately 24hours to complete onerotation. This has important environmental consequences. 1. Rotation creates a diurnal cycle

More information

Lornshill Academy. Geography Department Higher Revision Physical Environments - Atmosphere

Lornshill Academy. Geography Department Higher Revision Physical Environments - Atmosphere Lornshill Academy Geography Department Higher Revision Physical Environments - Atmosphere Physical Environments Atmosphere Global heat budget The earth s energy comes from solar radiation, this incoming

More information

Meteorology. Circle the letter that corresponds to the correct answer

Meteorology. Circle the letter that corresponds to the correct answer Chapter 6 Worksheet 2 Meteorology Name: Circle the letter that corresponds to the correct answer 1) A steep pressure gradient: a. produces light winds. b. produces strong winds. c. is only possible in

More information

Chapter 6: Atmospheric Pressure, Wind, and Global Circulation

Chapter 6: Atmospheric Pressure, Wind, and Global Circulation Discovering Physical Geography Third Edition by Alan Arbogast Chapter 6: Atmospheric Pressure, Wind, and Global Circulation Factors That Influence Air Pressure Air Pressure is the measured weight of air

More information

1 Currents. TAKE A LOOK 2. Read a Map In what direction does the Gulf Stream flow?

1 Currents. TAKE A LOOK 2. Read a Map In what direction does the Gulf Stream flow? CHAPTER 5 1 Currents SECTION The Movement of Ocean Water BEFORE YOU READ After you read this section, you should be able to answer these questions: What factors affect ocean currents? Why are ocean currents

More information

Wind and Wind Patterns

Wind and Wind Patterns Wind and Wind Patterns What is Weather? Weather is the condition of Earth s atmosphere at a particular time and place. What is Wind? Wind is air moving across the surface of the Earth. It can move horizontally

More information

Station 1: Solar Radiation on Earth

Station 1: Solar Radiation on Earth Station 1: Solar Radiation on Earth Activity Procedures 1. Choose one person to be the Sun. 2. Standing an arm s length away from the globe, have the Sun classmate hold the flashlight level with the equator,

More information

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa

Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa Foundations of Earth Science, 6e Lutgens, Tarbuck, & Tasa The Atmosphere in Motion Foundations, 6e - Chapter 13 Stan Hatfield Southwestern Illinois College Atmospheric pressure Force exerted by the weight

More information

McKnight's Physical Geography 11e

McKnight's Physical Geography 11e Chapter 2 Lecture McKnight's Physical Geography 11e Lectures Chapter 5 Atmospheric Pressure and Wind Michael Commons Ohio Northern University Atmospheric Pressure and Wind The Nature of Atmospheric Pressure

More information

Small- and large-scale circulation

Small- and large-scale circulation The Earth System - Atmosphere II Small- and large-scale circulation Atmospheric Circulation 1. Global atmospheric circulation can be thought of as a series of deep rivers that encircle the planet. 2. Imbedded

More information

Lesson: Ocean Circulation

Lesson: Ocean Circulation Lesson: Ocean Circulation By Keith Meldahl Corresponding to Chapter 9: Ocean Circulation As this figure shows, there is a connection between the prevailing easterly and westerly winds (discussed in Chapter

More information

6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of

6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of 6.9B verify through investigations that thermal energy moves in a predictable pattern from warmer to cooler 6.5B recognize that a limited number of elements comprise the largest portion of oceans and atmosphere

More information

Atmospheric Circulation (Ch. 8) Ocean & Atmosphere are intertwined Gases & waters freely exchanged Wind Weather Climate

Atmospheric Circulation (Ch. 8) Ocean & Atmosphere are intertwined Gases & waters freely exchanged Wind Weather Climate Atmospheric Circulation (Ch. 8) Ocean & Atmosphere are intertwined Gases & waters freely exchanged Wind Weather Climate Atmospheric Structure Consists of Layers Separated by Temperature Stratosphere: Temperature

More information

Atmospheric Circulation. Recall Vertical Circulation

Atmospheric Circulation. Recall Vertical Circulation Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and El Niño Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation

More information

Global Wind Paerns. specific. higher. convection. rises. rotates. equator Equatorial. Subtropical High. long. lower. troposphere. sinks.

Global Wind Paerns. specific. higher. convection. rises. rotates. equator Equatorial. Subtropical High. long. lower. troposphere. sinks. Global Wind Paerns Global Winds Winds that b steadily from direcons long over distances. specific Created by the of Earth s surface. Result of Sun striking the surface at angles near the equator and at

More information

Worldwide Wind 1-2 KEY CONCEPTS AND PROCESS SKILLS KEY VOCABULARY ACTIVITY OVERVIEW E-191

Worldwide Wind 1-2 KEY CONCEPTS AND PROCESS SKILLS KEY VOCABULARY ACTIVITY OVERVIEW E-191 Worldwide Wind 40- to 1-2 50-minute sessions ACTIVITY OVERVIEW COMPUTER 68 SIMUL ATION Students use a computer simulation to identify the most common wind direction in a particular location. They share

More information

ATMOSPHERIC CIRCULATION. WIND = The horizontal movement of air. Results from the differences in air pressure. Always moves from HIGH to LOW.

ATMOSPHERIC CIRCULATION. WIND = The horizontal movement of air. Results from the differences in air pressure. Always moves from HIGH to LOW. ATMOSPHERIC CIRCULATION WIND = The horizontal movement of air. Results from the differences in air pressure. Always moves from HIGH to LOW. Pressure differences result from variations in temperature. AIR

More information

Chapter 13 Lecture Outline. The Atmosphere in Motion

Chapter 13 Lecture Outline. The Atmosphere in Motion Chapter 13 Lecture Outline The Atmosphere in Motion Understanding Air Pressure Air pressure is the force exerted by weight of air above Weight of the air at sea level 14.7 psi or 1 kg/cm 2 Decreases with

More information

Lecture 5: Climate Tapestry. Sea/Land Breeze. Thermal Energy to Kinetic Energy

Lecture 5: Climate Tapestry. Sea/Land Breeze. Thermal Energy to Kinetic Energy Lecture 5: Climate Tapestry JS JP Thermal Energy to Kinetic Energy Hadley Cell Ferrel Cell (driven by eddies) Pressure and Wind Global Wind Patterns Polar Cell L H L H Effect of Earth s Rotation On Winds

More information

The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate.

The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate. The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate. In this lesson you will: 2.3.1 Define the term prevailing winds. (k) 2.3.3 State the impact

More information

Activity: Because the Earth Turns

Activity: Because the Earth Turns Activity: Because the Earth Turns Introduction: Almost everywhere on Earth (except at the equator), objects moving horizontally and freely (unconstrained) across Earth s surface travel in curved paths.

More information

3/22/11. General Circulation of the Atmosphere. General Circulation of the Atmosphere

3/22/11. General Circulation of the Atmosphere. General Circulation of the Atmosphere Chapter 10 General refers to the average air flow, actual winds will vary considerably. Average conditions help identify driving forces. The basic cause of the general circulation is unequal heating of

More information

GEOGRAPHY UNIT 2 REVIEW. 1. The daily atmospheric conditions, such as heat, moisture and air movement for a particular area are known as

GEOGRAPHY UNIT 2 REVIEW. 1. The daily atmospheric conditions, such as heat, moisture and air movement for a particular area are known as UNIT 2 REVIEW GEOGRAPHY Name: 1. The daily atmospheric conditions, such as heat, moisture and air movement for a particular area are known as 2. The average conditions of the weather for a long period

More information

Influences on Weather and Climate Weather and Climate. Coriolis Effect

Influences on Weather and Climate Weather and Climate. Coriolis Effect Influences on Weather and limate Weather and limate oriolis Effect 1 limate is defined as the common weather conditions in one area over a long period of time. Temperature, humidity, rainfall, and wind

More information

Horizontal movement of air between cooler and warmer regions. - horizontal movement of air Convection over areas where is

Horizontal movement of air between cooler and warmer regions. - horizontal movement of air Convection over areas where is Winds and Water Chapter 9 continued... Uneven Heating The various materials of the earth absorb and emit energy at different rates Convection Heated air expands; density reduced; air rises Upward movement

More information

PHSC 3033: Meteorology Air Forces

PHSC 3033: Meteorology Air Forces PHSC 3033: Meteorology Air Forces Pressure Gradient P/ d = Pressure Gradient (Change in Pressure/Distance) Horizontal Pressure Gradient Force (PGF): Force due to pressure differences, and the cause of

More information

Circulation of the Atmosphere

Circulation of the Atmosphere Circulation of the Atmosphere World is made up of three regions: Atmosphere (air) Hydrosphere (water) Lithosphere (land) - Geosphere All regions interact to produce weather (day to day variations) and

More information

Chapter 10: Global Wind Systems

Chapter 10: Global Wind Systems Chapter 10: Global Wind Systems Three-cell model of atmospheric circulation Intertropical Convergence Zone (ITCZ) Typical surface wind patterns Upper-level pressure and winds Climatological sea-level pressure

More information

The atmospheric circulation system

The atmospheric circulation system The atmospheric circulation system Key questions Why does the air move? Are the movements of the winds random across the surface of the Earth, or do they follow regular patterns? What implications do these

More information

Nevis Hulme Gairloch High School John Smith Invergordon Academy. Gairloch High School / Invergordon Academy

Nevis Hulme Gairloch High School John Smith Invergordon Academy. Gairloch High School / Invergordon Academy Nevis Hulme Gairloch High School John Smith Invergordon Academy 1 Gairloch High School / Invergordon Academy ATMOSPHERIC CIRCULATION The Three Cell Model Global Winds The ITCZ The purpose of this presentation

More information

The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate.

The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate. The student will be expected to demonstrate an understanding of the cause of winds and how winds affect climate. In this lesson you will: 2.3.1 Define the term prevailing winds. (k) 2.3.3 State the impact

More information

Write answers on your own paper. A. the Sun B. the Moon C. Earth s gravity D. Earth s rotation

Write answers on your own paper. A. the Sun B. the Moon C. Earth s gravity D. Earth s rotation The tmosphere Write answers on your own paper 1. What is the primary energy source that drives all weather events, including precipitation, hurricanes, and tornados?. the Sun. the Moon C. Earth s gravity

More information

Atmospheric Circulation. Density of Air. Density of Air: H 2 O and Pressure effects

Atmospheric Circulation. Density of Air. Density of Air: H 2 O and Pressure effects Today s topics: Atmospheric circulation: generation of wind patterns on a rotating Earth Seasonal patterns of climate: Monsoons and Sea Breezes Tropical Cyclones: Hurricanes and typhoons Atmospheric Circulation

More information

Introduction to Physical Oceanography STUDENT NOTES Date: 1. What do you know about solar radiation at different parts of the world?

Introduction to Physical Oceanography STUDENT NOTES Date: 1. What do you know about solar radiation at different parts of the world? Introduction to Physical Oceanography STUDENT NOTES Date: 1 Warm up What do you know about solar radiation at different parts of the world? What affect does the tilt of the Earth have on the northern and

More information

Ocean Currents that Redistribute Heat Globally

Ocean Currents that Redistribute Heat Globally Ocean Currents that Redistribute Heat Globally Ocean Circulation Ocean Currents Fig. CO7 OCEAN CURRENTS Surface ocean currents are similar to wind patterns: 1. Driven by Coriolis forces 2. Driven by winds

More information

Atmospheric & Ocean Circulation-

Atmospheric & Ocean Circulation- Atmospheric & Ocean Circulation- Overview: Atmosphere & Climate Atmospheric layers Heating at different latitudes Atmospheric convection cells (Hadley, Ferrel, Polar) Coriolis Force Generation of winds

More information

Chapter 9: Circulation of the Ocean

Chapter 9: Circulation of the Ocean Chapter 9: Circulation of the Ocean Tropical gardens on Britain s Scilly Isles. Only 48 kilometers (30 miles) off the coast of Cornwall at 50 N, these scenic islands lie in the path of the warm waters

More information

Section 6. The Surface Circulation of the Ocean. What Do You See? Think About It. Investigate. Learning Outcomes

Section 6. The Surface Circulation of the Ocean. What Do You See? Think About It. Investigate. Learning Outcomes Chapter 5 Winds, Oceans, Weather, and Climate Section 6 The Surface Circulation of the Ocean What Do You See? Learning Outcomes In this section, you will Understand the general paths of surface ocean currents.

More information

Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012.

Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012. Duckies have been found in Hawaii, Alaska, S. America, Scotland, Washington state and Australia as of 2012. We learned that it takes 3 years to complete one circuit of the North Pacific Gyre flow in the

More information

Traveling on a Rotating Sphere

Traveling on a Rotating Sphere Traveling on a Rotating Sphere Table of Contents Page Click the titles below to jump through the lesson 2 Spin-offs of a Rotating Sphere 3 What Do You Know? 3 Heated Fluid Circulation 4 Where Do The Trade

More information

Atmospheric & Ocean Circulation- I

Atmospheric & Ocean Circulation- I Atmospheric & Ocean Circulation- I First: need to understand basic Earth s Energy Balance 1) Incoming radiation 2) Albedo (reflectivity) 3) Blackbody Radiation Atm/ Ocean movement ultimately derives from

More information

El Niño Lecture Notes

El Niño Lecture Notes El Niño Lecture Notes There is a huge link between the atmosphere & ocean. The oceans influence the atmosphere to affect climate, but the atmosphere also influences the ocean, which can also affect climate.

More information

CHAPTER 6 Air-Sea Interaction

CHAPTER 6 Air-Sea Interaction CHAPTER 6 Air-Sea Interaction What causes Earth s seasons? Tilt (23.5 ) responsible for seasons 2011 Pearson Education, Inc. Distribution of Solar Energy Distribution of Solar Energy Atmosphere absorbs

More information

Wind is caused by differences in air pressure created by changes in temperature and water vapor content.

Wind is caused by differences in air pressure created by changes in temperature and water vapor content. Topic 8: Weather Notes, Continued Workbook Chapter 8 Wind is caused by differences in air pressure created by changes in temperature and water vapor content. Wind blows from high pressure areas to low

More information

Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 07. Lecture 14. Global Scale Winds. Simple Introductory Examples:

Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 07. Lecture 14. Global Scale Winds. Simple Introductory Examples: Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology

More information

Wind Energy. Definition of Wind Energy. Wind energy is energy from moving air.

Wind Energy. Definition of Wind Energy. Wind energy is energy from moving air. Wind Energy Definition of Wind Energy Wind energy is energy from moving air. Air has mass. When it moves, it has kinetic energy. Kinetic energy is the energy of motion. How does wind form? Wind forms when

More information