Length of day for a full year. Ocean Gyres. Wet. Adiabatic. lapse rate, starts at. dewpoint Dry Adiabatic lapse rate

Size: px
Start display at page:

Download "Length of day for a full year. Ocean Gyres. Wet. Adiabatic. lapse rate, starts at. dewpoint Dry Adiabatic lapse rate"

Transcription

1 Vernal Equinox March 20, 11:57 AM, CDT Sun will rise exactly in the east and set exactly in the west. All latitudes get 12 hours of day and 12 hours of dark. Length of day for a full year Wet Adiabatic Ocean Gyres lapse rate, starts at dewpoint Dry Adiabatic lapse rate January July What is water vapor. Can you see it? Two ways water vapor is important? Sargasso Sea Great Pacific Garbage Patch Centers of ocean gyres What is water vapor s role in redistributing energy from surplus to deficit areas of world? 1

2 ITCZ migration mbedded&v=qh011eayjaa This is a high definition animation of global air circulation created by the Community Climate System Model (CCSM) and the National Center for Atmospheric Research (NCAR). It spans one calendar year and is comprised of hourly data. Cloud cover is generally shown in white with areas of precipitation shown in orange. 3A, 21B, 33C, 9D The diagram to the lower right is the symbol for a (an) front. a). Cold b). Convergent c). Warm d). Occluded e). Stationary 9A, 27B, 39C, 15D When air is saturated all the following are true EXCEPT a). Content = capacity b). Evaporation rate is fast c). Relative humidity = 100% d). Air is at the dewpoint temperature 11A, 29B, 41C, 17D Why does the U.S. have more tornadoes than other countries? a. We have more trailer parks b. Our mountains run east to west c. Our mountains run north to south d. mt and ct air collide in early fall e. mt and mp air can collide in the central U.S 12A, 30B, 42C, 18D The monsoon and a land/sea breeze have which of the following in common? a). They are both local in scale b). They are both continental in scale c). They both result from unequal heating/cooling rates of land and water d). They both involve continuous southerly winds e). They both bring heavy rain to the affected area 14A, 32B, 2C, 20D The diagram to the right is of a pressure cell in the hemisphere. Arrows are air movement direction. a). Low, northern b). Low, southern c). High, southern d). High, northern 2

3 16A, 34B, 4C, 22D The South Atlantic Ocean Gyre rotates and brings relatively water to west coast of Africa. a). Clockwise, cold b). Counterclockwise, warm c). Clockwise, warm d). Counterclockwise, cold 17A, 35B, 5C, 23D A layered cloud is called a cloud, while a puffy cloud is called a cloud. a). Cirrus, Cumulus b). Stratus, Cirrus c). Nimbus, Stratus d). Cumulus, Nimbus e). Stratus, Cumulus 19A, 37B, 7C, 25D An air parcel that is forced up and over a mountain experiences which of the following temperature changes? a). Heats up at the dry adiabatic lapse rate as it descends on the leeward side b). Heats up due to friction as it goes up on the windward side of the mountain c). Cools off at the dry adiabatic lapse rate as it descends on the leeward side 23A, 41B, 11C, 29D A land breeze is likely to occur along the coast during the, due to relatively temperatures and atmospheric pressure over land. a). Night, low, high b). Night, high, low c). Day, low, high d). Day, high, low 24A, 42B, 12C, 30D In air mass names, if the lowercase first letter is m, it indicates that the airmass is, and if the capital second letter is P, it means the airmass is. a). Moist, cool b). Monsoon, Polar c). Moist, warm d). Dry, warm e). Marine, moist 25A, 1B, 13C, 31D If you were given the following altitudes and temperature readings from a weather balloon released into the atmosphere, what term would best describe this particular sequence of atmospheric temperature changes? a). Surface temperature inversion b). Wet adiabatic lapse rate c). Temperature inversion aloft d). Dry adiabatic lapse rate 3

4 29A, 5B, 17C, 35D On the weather map to the right the front labeled D is front and it is moving toward the. a). An occluded front, east b). A cold front, northeast c). A stationary front, south d). A warm front, northeast e). A cold front, east 30A, 6B, 18C, 36D The dry adiabatic lapse rate describes a). Temperature changes in a rising parcel of air with condensation occurring b). Temperature changes associated with falling parcels of air c). Temperature structure of the atmosphere 31A, 7B, 19C, 37D The ratio of atmospheric water vapor content to atmospheric water vapor capacity is called a). Adiabatic rate b). Transpiration ratio c). Saturation curve d). Relative humidity e). Condensation level 32A, 8B, 20C, 38D In December, the ITCZ is usually located the Equator because a). On, there are always equal days and equal nights b). South of, the direct rays of the sun shine on the Tropic of Capricorn c). North of, the direct rays of the sun shine on the Tropic of Cancer d). North of, the direct rays of the sun shine on the Arctic Circle e). South of, the direct rays of the sun shine on the Antarctic Circle 36A, 12B, 24C, 42D A cold front passes through Mobile, you might expect all the following EXCEPT a). Cumulonimbus clouds b). Stratus clouds and drizzle c). The temperature to change rapidly d). Heavy rain e). Rapid atmospheric pressure changes 37A, 13B, 25C, 1D The type of atmospheric lifting that causes rainfall near the Equator is lifting. a). Frontal b). Orographic c). Divergent d). Advective e). Convergent 4

5 39A, 15B, 27C, 3D A hurricane is wandering around in the Gulf of Mexico. It finally heads due east towards Florida. Use the map to right to determine what quadrant of the storm will do the most damage to Florida s western coast. a). Northeast quadrant b). Northwest quadrant c). Southeast quadrant d). Southwest quadrant Driver Front seat passenger 40A, 16B, 28C, 4D Global average precipitation is low near the Poles because air temperature is, capacity of air to hold water is, and provides a lifting mechanism. a). Warm, low, convergence b). Cold, high, nothing c). Warm, low, convection d). Cold, low, nothing e). Cold, low, frontal activity 41A, 17B, 29C, 5D Condensation is affected by all the following EXCEPT a). Degree of cooling b). Type of vegetation c). Relative humidity d). Availability of condensation nuclei e). Ratio of moisture content to capacity 42A, 18B, 30C, 6D In comparison to the idealized pattern of high and low pressure belts, the actual global pressure distribution is all the following EXCEPT a). The pattern is much more irregular because of continentality b). In June, the ITCZ is usually south of the equator c). The pressure belts break up into large pressure cells especially in the northern hemisphere d). The pressure belts are more zonal in the southern hemisphere than in the northern hemisphere e). In December, a high pressure cell is over Siberia in Russia 43AC What is the correct descriptive term for belt #2? a) Horse Latitudes b) Westerlies c) Southeast trades d) Polar Easterlies e) Polar Front 44AC What is the correct descriptive term for belt #4? a) Polar Easterlies b) Horse Latitudes c) Westerlies d) Southeast trades e) Northeast trades 5

6 46AC What is(are) the correct descriptive term(s) for belt #7? a) Doldrums b) Subtropical High c) Equatorial Low d) ITCZ e) all but b 48AC What is(are) the correct descriptive term(s) for belt #11? a) Horse Latitudes b) Polar Front c) Polar High d) Subpolar Low e) b and d 50 AC The surface winds in zone #4 usually come from the a) North b) Southwest c) Northeast d) East e) Northwest 52AC The surface winds in zone #12 usually come from the a) Southeast b) North c) Northeast d) West e) Northwest 54AC What is the atmospheric pressure at location 3 and what causes it? a) high pressure caused by circulation dynamics b) low pressure caused by circulation dynamics c) low pressure caused by cold temperatures d) high pressure caused by low temperatures 54BD What is the atmospheric pressure at location #9 and what causes it? a). high pressure caused by warm temperatures b). high pressure caused by circulation dynamics c). low pressure caused by warm temperatures d). low pressure caused by circulation dynamics 6

7 Latitudinal variation in precipitation 59AC If we ranked annual precipitation with the greatest amount of precipitation as A, next to greatest B, next to lowest C, and lowest D, which of these four ranks best describes precipitation in location #11? a) A, greatest amount of precipitation b) B, next to greatest c) C, next to lowest d) D, lowest Know the lifting mechanisms, or lack thereof, that explain this latitudinal pattern 59BD If we ranked annual precipitation with the greatest amount of precipitation as A, next to greatest B, next to lowest C, and lowest D, which of these four ranks best describes precipitation in location #5? a). A, greatest amount of precipitation b). B, next to greatest c). C, next to lowest d). D, lowest 7

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

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

WEATHER SYSTEMS OF MIDDLE LATITUDES

WEATHER SYSTEMS OF MIDDLE LATITUDES CHAPTER 10 WEATHER SYSTEMS OF MIDDLE LATITUDES MULTIPLE CHOICE QUESTIONS 1. In equal volumes, which one of the following air masses exerts the highest surface air pressure? a. cp *b. A c. mp d. ct e. mt

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

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

Weather EOG Review Questions

Weather EOG Review Questions Weather EOG Review Questions 1. Which statement best describes runoff? A Water vapor cools off and changes into water droplets. B Water in the form of rain, snow, sleet, or hail falls from clouds. C Precipitation

More information

Meteorology. Circle the letter that corresponds to the correct answer

Meteorology. Circle the letter that corresponds to the correct answer Chapter 7 Worksheet 2 Meteorology Name: Circle the letter that corresponds to the correct answer 1) Which of the following factors contributes to the general subsidence in the latitude zone 20 degrees

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

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

Envs, Geol, Phys 112: Global Climate. Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10

Envs, Geol, Phys 112: Global Climate. Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10 Exam 1 Review Energy-Atmosphere System Review Aguado & Bert, Ch. 1, 2, 3, 4, 5, 6, 9, 10 Location on Earth (L04) Latitude & Longitude great circles, prime meridian, time zones, cardinal points, azimuth

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

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

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

Meteorology I Pre test for the Second Examination

Meteorology I Pre test for the Second Examination Meteorology I Pre test for the Second Examination MULTIPLE CHOICE 1. A primary reason why land areas warm up more rapidly than water areas is that a) on land, all solar energy is absorbed in a shallow

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

Global Wind and Pressure Belts as a Response to the Unequal Heating of the Atmosphere

Global Wind and Pressure Belts as a Response to the Unequal Heating of the Atmosphere GRADE 11 GEOGRAPHY SESSION 3: GLOBAL AIR CIRCULATION Key Concepts In this lesson we will focus on summarising what you need to know about: The mechanics present to create global wind and pressure belts

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

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

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

LAB H - ATMOSPHERE AND CLIMATE LAB II STABILITY AND PRECIPITATION PATTERNS

LAB H - ATMOSPHERE AND CLIMATE LAB II STABILITY AND PRECIPITATION PATTERNS Introduction LAB H - ATMOSPHERE AND CLIMATE LAB II STABILITY AND PRECIPITATION PATTERNS This lab will provide students with the opportunity to become familiar with the concepts of atmospheric stability

More information

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

Higher Atmosphere. Earth s Heat Budget. Global Insolation. Global Transfer Of Energy. Global Temperatures. Inter Tropical Convergence Zone Higher Atmosphere Earth s Heat Budget Global Insolation Global Transfer Of Energy Global Temperatures Inter Tropical Convergence Zone Climate Graph Earth s Heat Budget Task 1 Use the Power Point to help

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

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

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

Chapter 7: Circulation And The Atmosphere

Chapter 7: Circulation And The Atmosphere Chapter 7: Circulation And The Atmosphere Highly integrated wind system Main Circulation Currents: series of deep rivers of air encircling the planet Various perturbations or vortices (hurricanes, tornados,

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

Air Masses and Fronts. Holt Science and Technology Weather and Climate Chapter 2, Section 2

Air Masses and Fronts. Holt Science and Technology Weather and Climate Chapter 2, Section 2 Air Masses and Fronts Holt Science and Technology Weather and Climate Chapter 2, Section 2 Types of Air Masses Changes in weather are caused by the movement and interaction of air masses. An air mass is

More information

8 th Grade Science Meteorology Review

8 th Grade Science Meteorology Review 8 th Grade Science Meteorology Review #1 Where does Earth get the energy that produces global weather patterns? A: The sun B: Humidity C: Air masses D: Cyclones A. The Sun #2 Do all of the areas on Earth

More information

Global Weather Patterns

Global Weather Patterns Global Weather Patterns AZ State Standards Concept 2: Energy in the Earth System (Both Internal and External) Understand the relationships between the Earth s land masses, oceans, and atmosphere. PO 2.

More information

In Search of the Source of Wind.

In Search of the Source of Wind. In Search of the Source of Wind Role of Wind in the Voyage Atmospheric Pressure The Weight of Atmospheric Air on Earth Gravitational force helps Air to remain on Earth Variations in the Atmospheric Pressure

More information

Lecture Outlines PowerPoint. Chapter 18 Earth Science 11e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 18 Earth Science 11e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 18 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

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

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

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

1.3: CLIMATE GEOGRAPHY. pgs

1.3: CLIMATE GEOGRAPHY. pgs 1.3: CLIMATE GEOGRAPHY pgs. 76-89 INTRODUCTION WEATHER: Is the combination of temperature, precipitation, cloud cover and wind that we experience EACH DAY. Example: 22 0 C and clear skies. CLIMATE: The

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

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

Wednesday, September 15, 2010 Coriolis force, 3 dimensions (p 65)

Wednesday, September 15, 2010 Coriolis force, 3 dimensions (p 65) Wednesday, September 15, 2010 Coriolis force, 3 dimensions (p 65) Weather fronts (p 63) General circulation on a rotating Earth (p 65) Geostrophy force balance (p 66) Local effects (no coriolis 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

AT350 EXAM #2 November 18, 2003

AT350 EXAM #2 November 18, 2003 AT350 EXAM #2 November 18, 2003 Name and ID: Enter your name and student ID number on the answer sheet and on this exam. Record your answers to the 50 questions by using a No. 2 pencil to completely fill

More information

Weather & Atmosphere Study Guide

Weather & Atmosphere Study Guide Weather & Atmosphere Study Guide 1. Draw a simple water cycle diagram using the following words: Precipitation, Evaporation, Condensation, Transpiration 2. In your own words, explain the difference between

More information

Exit Ticket: Coriolis Effect

Exit Ticket: Coriolis Effect Exit Ticket: Coriolis Effect 1. How does the Coriolis Effect influence the path of projectiles or wind traveling through the atmosphere? Causes them to curve 2. In which direction does the Coriolis Effect

More information

ESCI 107 The Atmosphere Lesson 11 Global Circulation

ESCI 107 The Atmosphere Lesson 11 Global Circulation Reading: Meteorology Today, Chapter 10 THE GLOBAL CIRCULATION ESCI 107 The Atmosphere Lesson 11 Global Circulation Latitudinal heat imbalance The tropics receive more radiation than they emit. The polar

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

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

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

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

Chapter 8 Air Masses

Chapter 8 Air Masses Chapter 8 Air Masses Air Masses - 1 1. An Air Mass is a large body of air usually about 1500 km across and several km thick, that has homogeneous physical properties. 2. The important physical properties

More information

Topic 4 Temperature, Atmospheric Circulation and Climate. Temperature Concepts and Measurement 10/2/2017. Thermometer and Instrument Shelter

Topic 4 Temperature, Atmospheric Circulation and Climate. Temperature Concepts and Measurement 10/2/2017. Thermometer and Instrument Shelter Topic 4 Temperature, Atmospheric Circulation and Climate Temperature Controls Global Temp. Patterns Atmospheric Circulation Primary High and Low Pressure Areas Global Circulation Model Local Winds Ocean

More information

Lecture 13 March 24, 2010, Wednesday. Atmospheric Pressure & Wind: Part 4

Lecture 13 March 24, 2010, Wednesday. Atmospheric Pressure & Wind: Part 4 Lecture 13 March 24, 2010, Wednesday Atmospheric Pressure & Wind: Part 4 Synoptic scale winds Mesoscale winds Microscale winds Air-sea interactions The largest synoptic scale wind. Monsoon: Arabic for

More information

TOPICS YOU NEED TO KNOW

TOPICS YOU NEED TO KNOW ATMO 101 Introduction to Meteorology Midterm Study Sheet Chapters 6, 7, 8 and 10 Exam Thursday 3/23/2017 Vocabulary Words for True and False, and Multiple Choice You are responsible for the following words:

More information

9. The Earth's planetary winds are deflected as a result of the Earth's A) revolution around the Sun B) seasonal changes C) rotation on its axis D)

9. The Earth's planetary winds are deflected as a result of the Earth's A) revolution around the Sun B) seasonal changes C) rotation on its axis D) 1. Which ocean current transports warm water away from Earth s equatorial region? A) Brazil Current B) Guinea Current C) Falkland Current D) California Current 2. The Gulf Stream and North Atlantic Current

More information

Enviro Sci 1A03 Quiz 3

Enviro Sci 1A03 Quiz 3 Enviro Sci 1A03 Quiz 3 Question 1 (1 point) Which of the following measure wind direction and speed? Question 1 options: a) aerovane b) anemometer c) wind vane d) all of the above Question 2 (1 point)

More information

Introduction to Oceanography OCE 1001

Introduction to Oceanography OCE 1001 Introduction to Oceanography OCE 1001 Lecture Notes Chantale Bégin & Jessica Fry Version 2.1 10. Ocean Circulation (Trujillo, Chapter 7) Major ocean currents are stable and predictable; they have been

More information

Weather and Climate. Climate the situation of the atmosphere during a long period of time and a big surface.

Weather and Climate. Climate the situation of the atmosphere during a long period of time and a big surface. Weather and Climate Weather and Climate Weather the situation of the atmosphere during a short period of time and a small surface of the Earth. It is very irregular and changes a lot. Climate the situation

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 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

Canada s vast size creates a diverse range of weather conditions and climatic conditions. Warming trend for last 10 years Wet Spring Dry five summers

Canada s vast size creates a diverse range of weather conditions and climatic conditions. Warming trend for last 10 years Wet Spring Dry five summers Chapter 4 Weather and Climate Canada s vast size creates a diverse range of weather conditions and climatic conditions. Weather examples: Rainy today Snow tomorrow Fog on Wednesday 23 degree C today High

More information

Social Studies CHAPTER 2: PART 2 CLIMATE AND WEATHER

Social Studies CHAPTER 2: PART 2 CLIMATE AND WEATHER Social Studies CHAPTER 2: PART 2 CLIMATE AND WEATHER Climate Weather and Identity Climate and weather have a large influence on how Canadians build their identity. We will study the factors that contribute

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

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

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

THE ATMOSPHERE. WEATHER and CLIMATE. The Atmosphere 10/12/2018 R E M I N D E R S. PART II: People and their. weather. climate?

THE ATMOSPHERE. WEATHER and CLIMATE. The Atmosphere 10/12/2018 R E M I N D E R S. PART II: People and their. weather. climate? R E M I N D E R S Two required essays are due by Oct. 30, 2018. (A third may be used for extra credit in place of a Think Geographically essay.) ESSAY TOPICS (choose any two): Contributions of a noted

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

Water Budget I: Precipitation Inputs

Water Budget I: Precipitation Inputs Water Budget I: Precipitation Inputs Forest Cover Global Mean Annual Precipitation (MAP) Biomes and Rainfall Forests won t grow where P < 15 / yr Forest type depends strongly on rainfall quantity, type

More information

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

9/25/2014. Scales of Atmospheric Motion. Scales of Atmospheric Motion. Chapter 7: Circulation of the Atmosphere Chapter 7: Circulation of the Atmosphere The Atmosphere: An Introduction to Meteorology, 12 th Lutgens Tarbuck Lectures by: Heather Gallacher, Cleveland State University Scales of Atmospheric Motion Small-

More information

Land and sea breezes are an example of which type of heat transfer?

Land and sea breezes are an example of which type of heat transfer? TEST #7 REVIEW Land and sea breezes are an example of which type of heat transfer? Land and sea breezes are an example of which type of heat transfer? convection The diagram above represents what? The

More information

Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are.

Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are. Name Date L.O: SWBAT explain what breezes, planetary winds, ocean currents & monsoons are. 1. A cool breeze is blowing toward the land from the ocean on a warm, cloudless summer day. This condition is

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

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

Weather Unit Study Guide

Weather Unit Study Guide Weather Unit Study Guide - 2018 Weather vs Climate What does weather measure? The condition of the earth's atmosphere at a particular time and place. How are climate and weather different? Climate is the

More information

Applied Earth Science Climate Exam Practice Questions Page 1

Applied Earth Science Climate Exam Practice Questions Page 1 Name: 1. Which combination of climate factors generally results in the coldest temperatures? A) low elevation and low latitude B) low elevation and high latitude C) high elevation and low latitude D) high

More information

PHYSICAL GEOGRAPHY. By Brett Lucas

PHYSICAL GEOGRAPHY. By Brett Lucas PHYSICAL GEOGRAPHY By Brett Lucas ATMOSPHERIC PRESSURE AND WIND Atmospheric Pressure and Wind Atmospheric Processes The Nature of Wind General Circulation of the Atmosphere Modifications of General Circulation

More information

Winds and Ocean Circulations

Winds and Ocean Circulations Winds and Ocean Circulations AT 351 Lab 5 February 20, 2008 Sea Surface Temperatures 1 Temperature Structure of the Ocean Ocean Currents 2 What causes ocean circulation? The direction of most ocean currents

More information

Ocean Currents Lecture Notes

Ocean Currents Lecture Notes Ocean Currents Lecture Notes (Topic 9A) page 1 Ocean Currents Lecture Notes Surface Currents Ocean Currents (What is an ocean current? How is a current different from a wave?) The water in an travels from

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

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

- wet tropical climate

- wet tropical climate (1 of 13) Further Reading: Chapter 10 of the text book Outline - wet tropical climate - coastal trade wind climate - wet-dry and monsoon climate - dry tropical climate (2 of 13) Introduction Previously,

More information

Notepack 41. Aim: What factors determine the climate of a certain area? Do Now: What is the difference between weather and climate?

Notepack 41. Aim: What factors determine the climate of a certain area? Do Now: What is the difference between weather and climate? Notepack 41 Aim: What factors determine the climate of a certain area? Do Now: What is the difference between weather and climate? WEATHER VS. CLIMATE Weather atmospheric conditions at a certain location

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

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

First of all, you should know that weather and climate are not the same thing.

First of all, you should know that weather and climate are not the same thing. First of all, you should know that weather and climate are not the same thing. WEATHER IS: Short term Limited area Can change rapidly Difficult to predict WEATHER is what s happening outside your window

More information

Water in the Atmosphere

Water in the Atmosphere Water in the Atmosphere Chapter 24 Solid to Liquid The process of changing state, such as melting ice, requires that energy be transferred in the form of heat. Latent heat is the energy absorbed or released

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

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

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

Announcements. Why does the wind blow? What makes the ocean flow? Pressure gradients and Coriolis. First assignment (deep-sea sediments)

Announcements. Why does the wind blow? What makes the ocean flow? Pressure gradients and Coriolis. First assignment (deep-sea sediments) Announcements First assignment (deep-sea sediments) I expect to be finished grading exams in two weeks. Second problem set due November 7th New topic: Physics of atmospheric and oceanic circulation Atmospheric

More information

Unit Test Study Guide:

Unit Test Study Guide: Name: Homeroom: Date: Unit 6: Meteorology Study Guide Unit Test Study Guide: Atmosphere & Weather Use the summary points below as a resource to help you study for our unit test Monday! EARTH S ATMOSPHERE:

More information

LAB H - ATMOSPHERE AND CLIMATE LAB II STABILITY AND PRECIPITATION PATTERNS

LAB H - ATMOSPHERE AND CLIMATE LAB II STABILITY AND PRECIPITATION PATTERNS Introduction LAB H - ATMOSPHERE AND CLIMATE LAB II STABILITY AND PRECIPITATION PATTERNS This lab will provide students with the opportunity to become familiar with the concepts of atmospheric stability

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

Understanding Weather

Understanding Weather Understanding Weather Images Graphic of the atmosphere. Enlarge Cirrus clouds. Enlarge Air masses Air masses are parcels of air that bring distinctive weather features to the country. An air mass is a

More information

Unit 2 World Climate Patterns

Unit 2 World Climate Patterns Unit 2 World Climate Patterns Weather the day to day or short term conditions of the atmosphere. Weather includes variables such as temperature, precipitation, humidity, cloud cover, wind, and air pressure.

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

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

The General Circulation and El Niño. Dr. Christopher M. Godfrey University of North Carolina at Asheville The General Circulation and El Niño Dr. Christopher M. Godfrey University of North Carolina at Asheville Global Circulation Model Air flow broken up into 3 cells Easterlies in the tropics (trade winds)

More information

Warm front and cold front video 3:50

Warm front and cold front video 3:50 Construct an explanation of the relationship between air pressure, weather fronts, and air masses and meteorological events such as tornados and thunderstorms Unpacked : Warm front and cold front video

More information

Review for the second quarter. Mechanisms for cloud formation

Review for the second quarter. Mechanisms for cloud formation Review for the second quarter Mechanisms for cloud formation 1 Rising air expands and cools; Sinking air compresses and warms. (18) (24) Dry adiabatic lapse rate (10 o C/km): the rate of temperature decrease

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

>>>>>>>>WHEN YOU FINISH <<<<<<<< Hand in the answer sheet separately.

>>>>>>>>WHEN YOU FINISH <<<<<<<< Hand in the answer sheet separately. Instructor: Prof. Seiberling PHYSICS DEPARTMENT MET 1010 2nd Midterm Exam October 28, 2002 Name (print, last rst): Signature: On my honor, I have neither given nor received unauthorized aid on this examination.

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