Trade winds Prevailing westerlies east

Similar documents
Warm-up. color mass. albedo. mirage

Section 3: Atmospheric Circulation

Wind and Air Pressure

3 Global Winds and Local Winds

3 Global Winds and Local Winds

Global Winds and Local Winds

Atmosphere Circulation

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

Earth s Atmosphere. Air Currents

Atmosphere & Weather. Earth Science

Atmospheric Circulation

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

Full Name: Class: Period: Date:

Local and Global Winds

CHAPTER 6 Air-Sea Interaction

Lecture The Oceans

3 Global Winds and Local Winds

Wind and Wind Patterns

Wind Patterns on Earth

Finish Characteristics of Climate

Lesson: Atmospheric Dynamics

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

Chapter 6: Atmospheric Pressure, Wind, and Global Circulation

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

Prevailing Winds. The Coriolis Effect

ATOMOSPERIC PRESSURE, WIND & CIRCULATION

Air Pressure and Wind

Earth s Atmosphere. Atmospheric Gases. Other Gases. Solids in the Atmosphere

Chapter: Atmosphere Section 3: Air Movement

8 th Grade Science Meteorology Review

Atmospheric Gases. Earth s Atmosphere extends from earth s surface to outer space. It is made up of a mixture of gases with some solids and liquids.

Chapter. Air Pressure and Wind

W3 Global Circulation Systems

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

Weather & Atmosphere Study Guide

I. Atmosphere. Maintains a balance between the amount of heat absorbed from the Sun and the amount of heat that escapes back into space.

Enviro Sci 1A03 Quiz 3

Lornshill Academy. Geography Department Higher Revision Physical Environments - Atmosphere

Atmospheric & Ocean Circulation-

EARTH SCIENCE 5.9 (WIND) WEATHER

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

OCN 201 Surface Circulation

Meteorology I Pre test for the Second Examination

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

Weather Unit Study Guide

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

The Coriolis Effect - Deflect the Arrows!

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

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

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

McKnight's Physical Geography 11e

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

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

Wind in the Atmosphere

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

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

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

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

ESCI 107 The Atmosphere Lesson 11 Global Circulation

Exit Ticket: Coriolis Effect

9/25/2014. Scales of Atmospheric Motion. Scales of Atmospheric Motion. Chapter 7: Circulation of the Atmosphere

Earth s Atmosphere. Earth s atmosphere is a key factor in allowing life to survive here.

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

Station 1: Solar Radiation on Earth

Atmospheric & Ocean Circulation- I

Chapter: Atmosphere Section 3: Air Movement

Wind Movement and Global and Local Winds

Carolina TM Coriolis Effect and Atmospheric Circulation Kit STUDENT GUIDE

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

Global Winds AOSC 200 Tim Canty

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

Chapter 7 Weather and Climate

Influences on Weather and Climate Weather and Climate. Coriolis Effect

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

Chapter 10: Global Wind Systems

Chapter 13 Lecture Outline. The Atmosphere in Motion

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

Higher Atmosphere. Earth s Heat Budget. Global Insolation. Global Transfer Of Energy. Global Temperatures. Inter Tropical Convergence Zone

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

Atmospheric Circulation. Recall Vertical Circulation

The General Circulation and El Niño. Dr. Christopher M. Godfrey University of North Carolina at Asheville

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

Meteorology. Circle the letter that corresponds to the correct answer

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

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

The atmospheric circulation system

Wind in the Atmosphere

Small- and large-scale circulation

PHYSICAL GEOGRAPHY. By Brett Lucas

10.2 Energy Transfer in the Atmosphere

Greenhouse Effect Activity

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

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

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

Ecology. Professor Andrea Garrison Biology 3A Illustrations 2014 Cengage Learning unless otherwise noted

Exploring Wind Energy

Factors Affecting Wind

Circulation of the Atmosphere

Circulation Patterns

Warm-Up Please write down these questions and leave space to answer them. (Do not answer them yet)

Transcription:

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, 3.What direction do the winds from the polar regions come from? east

Warm-up Page: 527, 1. The Circulation of the atmosphere and the oceans is affected by the of the Earth on its axis. rotation Page: 527, 2. The tendency of moving objects to follow curved paths rather than straight line due to Earth rotation is called the Coriolis effect Page: 528, 3. Looping patterns of air flow as hot air rises, and cool air sinks is called an Convection cell or current

Warm-up quiz 1. The fraction of solar radiation reflected from an object is called the. 2. The transfer of energy as heat from one substance to another by direct contact is called. 3. What layer of the atmosphere do we live in? 4. What is the major wind belt that most of the USA belongs to: 5. The Circulation of the atmosphere and the oceans is affected by the of the Earth on its axis.

Objective: S.W.B.A.T. Describe the global patterns of air circulation, and name three global wind belts. Identify two factors that form local wind patterns. Explain the Coriolis effect. Create a model and booklet on global wind patterns Show how energy and matter flow in cycles in wind belts Use model booklet to answer question related to wind belts

Activities: Warm-up Creat wind belt book Complete questions Color code wind belts Communicate information/questions answered

Atmospheric Circulation Sec. 19-3

How Air Moves Differences in air pressure are caused by unequal heating of Earth s surface.(causing convection) Hot air is rising at the equator creating a low pressure area. Cold air is sinking at both poles causing high pressure areas.

Air moves from areas of high pressure to areas of low pressure, causing a general, worldwide movement of surface air from the poles toward the equator. This, along with the Coriolis effect, creates wind patterns.

The Coriolis Effect Coriolis effect - the curving of the path of a moving object from an otherwise straight path due to Earth s rotation The Coriolis effect causes winds to be deflected by Earth s rotation. http://wn.com/what's_t he_coriolis_effect? Wi nds BBC_Fou

Each hemisphere contains three looping patterns of flow called convection cells. Global Winds

Global Winds Each convection cell correlates to an area of Earth s surface, called a wind belt, that is characterized by winds that flow in one direction. These winds are called prevailing winds. Winds are named from where the come from

1 st Global Wind Belt 1. Trade Winds the prevailing winds that blow from east to west from +/- 30º latitude to the equator in both hemispheres Trade Winds Inter-Tropical Convergence Zone Trade Winds

Doldrums area of rising air at the equator, where the surface winds are weak Sailing vessels sometimes would get trapped of days.

2 nd Global Wind Belt 2. Westerlies - prevailing winds that blow from west to east between 30º and 60º latitude in both hemispheres Polar Easterlies Westerlies Trade Winds Intertropical Convergence Zone Trade Winds Westerlies Polar Easterlies

Global Winds Jet Streams are a narrow band of strong winds that blow in the upper troposphere & lower stratosphere These wind exist in the Northern and Southern Hemispheres. they direct paths of weather

3 rd Global wind belt 3. Polar easterlies caused by cool air descending (sinking) from the poles and is turned by the Coriolis effect. Winds move from east to west

Global Winds

Cool down 1. The doldrums are located between what wind belts in north and south? Trade winds 2. What are the names of the bands of high winds in the upper troposphere that are created from the global wind pattern jet streams