General Oceanography Geology 105 Expedition #19 The Ocean and Climate

Size: px
Start display at page:

Download "General Oceanography Geology 105 Expedition #19 The Ocean and Climate"

Transcription

1 General Oceanography Geology 105 Expedition #19 The Ocean and Climate Name Not attempting to answer questions on expeditions will result in point deductions on course workbook (two or more blank answers will result in a deduction of 2-4 points; a 5 point deduction will be assessed if more than five answers are left blank). Objective: Establish the link between ocean circulation and climate First we will examine the boundary currents, both the western and eastern, since examples of each impacts the climate of the United States, as well as many other nations in the world. Second we will look at coastal upwelling along central and northern California, which has a powerful effect on the climate in the bay area and operates on seasonal time-scale. And third, we will look at the global conveyor belt, a combination of deep (thermohaline) circulation and surface, wind-driven circulation that transports heat through the oceans causing major climatic effects on a time-scale of decades, centuries and millennia. 1. Introduction - Ocean and Climate Why is the ocean used to forecast the long-range weather? How might global warming affect the ocean and climate? General Oceanography, GEOL 105, Summer 2012 Session II Page 205 of

2 2. The California Current - And It's Not Some Trendy Bistro! --Jim Bettinger Draw an arrow on the map below showing the flow direction of the California current What effect does this current have on climate along northern and central California? 3. Current Marine Conditions - let's examine the today's conditions at several buoys (floats) with instruments - Complete by the table below - Note that station is in the open ocean whereas the other stations are closer to the coast. If station is not yet operational, then go into sea temperature listed below Climatic summary table line and determine the average sea temperature for this month from the graph (midpoint on red line). Do the same thing for air temperature, and put these under in the table below. Real-Time Observation ) Latitude 2) Longitude 3) Location Description 4) Air temperature 5) Water temperature General Oceanography, GEOL 105, Summer 2012 Session II Page 206 of

3 On the map above, draw a pattern of your choice in the regions of the coldest surface water 4. Acquiring Data on the Wind By means of arrows, show the prevailing wind direction off California during the spring and summer General Oceanography, GEOL 105, Summer 2012 Session II Page 207 of

4 5. Making a Model Let s examine the wind and surface water flow in the coastal ocean Make two diagrams (depth view and top view) showing the direction of water motion in the Ekman layer below the wind. 6. Why is the water at the coast so cold along California? We now have the two pieces of puzzle..think eastern boundary currents first and then cold, rising water Give two reasons for the cold sea surface temperature off central and northern California a. b. Put arrows on the drawing below to show the combination of the south-flowing California current and coastal upwelling, in addition to the prevailing wind direction along the California coast in the spring and summer North Ocean Coast Land General Oceanography, GEOL 105, Summer 2012 Session II Page 208 of

5 7. Other Aspects of Upwelling How do the ocean conditions set up by the eastern boundary currents encourage upwelling? What other regions of the ocean exhibit upwelling? 8. Monterey Bay National Marine Sanctuary Let s move to the south into the neighboring Monterey Bay National Marine Sanctuary. How does upwelling set the framework for the marine ecosystem along California? 9. Upwelling and Regional Climate How does upwelling influence the climate along the coastline of northern and central California, especially during the spring and summer months? General Oceanography, GEOL 105, Summer 2012 Session II Page 209 of

6 10. Combining Surface Circulation with Deep Circulation - the Global Conveyor Belt What is the driving force behind circulation of the deep waters? What is one technique use to track the deep currents? 11. Influence of the Conveyor Belt How does the deep circulation influence life on our planet? 12. Tracking Deep Ocean Current Let s Deploy Argo Floats Describe three ways that you will use to track the flow of deep water (thermohaline) circulation a. b, c. 13. Let s Ride the Global Conveyor Belt Using the methods described on the previous problem, let s track the deep water movement. What property is being used as a tracer in this example? General Oceanography, GEOL 105, Summer 2012 Session II Page 210 of

7 Use your research during the rest of the expedition to draw the global ocean conveyor on the map below with different colored pencils; use orange or red arrows for the direction of the warm surface currents (orange or red) and blue or purple arrows for the cold, salty deep currents Global Map General Oceanography, GEOL 105, Summer 2012 Session II Page 211 of

8 Why does the ocean have a high salinity in the North Atlantic? Draw on the global map, the flow of the Gulf Stream into the north Atlantic and into the Norwegian-Greenland Sea and also the flow of high salinity water out of the Mediterranean Sea. 14. Mischief in the Norwegian-Greenland Sea How might the sinking of North Atlantic Deep Water (NADW) in the Norwegian- Greenland Sea influence the global climate? Make a diagram of the flow of "warm, salty" water into the North Atlantic and the sinking of cold, salty, oxygen-rich water in the Norwegian-Greenland Sea 0 meters Equator Sea Surface Greenland Seafloor Water Depth 4000 meters Seafloor General Oceanography, GEOL 105, Summer 2012 Session II Page 212 of

9 If the ice mass in Greenland continues to melt (see audio clip), how might this influence the salinity of the ocean water in the Norwegian-Greenland Sea, and how might this influence the ability of surface water to sink, and thereby the global conveyor belt? 15. Into the South Atlantic - remember to show the flow of water into the south Atlantic on the global map from both the north and south Use the diagram below to show how oxygen-rich deep water is provided to the south Atlantic? Label the NADW and AABW water masses. 0 meters Antarctica Sea Surface Equator Greenland Water Depth 4000 meters Seafloor Surface Latitude 16. Into the Indian Ocean - remember to show the flow of deep water into the Indian Ocean on the global map What happens to the deep water flow of the conveyor belt in the Indian Ocean? General Oceanography, GEOL 105, Summer 2012 Session II Page 213 of

10 17. Into the South Pacific - remember to continue your diagram on the global map Describe what happens to the flow of the conveyor belt in the Pacific Ocean. 18. Into the North Pacific - remember to continue your diagram on the global map Where does the global conveyor belt go after mixing with intermediate and shallow water in the north Pacific? 19. Through the Philippines and Indonesia and into the Indian Ocean - continue on your global page (I studied this portion of the conveyor as a portion of my doctoral work) 20. Across the Indian Ocean - continue your global map How do surface currents (see your surface circulation map in the previous expedition) assist in the westward flow of the conveyor belt in the Indian Ocean? General Oceanography, GEOL 105, Summer 2012 Session II Page 214 of

11 21. Back into the Atlantic Ocean - continue your global map How does the water of the conveyor belt make its way back into the north Atlantic Ocean? 22. As we gain more knowledge, simple models often become more complex. Explain how recent work is leading to a modification of ideas on the southward flow of deep water in the north Atlantic. 23. Ignoring the Science and Misinterpreting Scientific Results Explain how recent work has been misinterpreted for political means, rather than science. 24. Let s Join Dr. Ruth Curry in a Simple Experiment on Climate Change and the Ocean What does this experiment say about the role of sea ice and the ocean in climate change? General Oceanography, GEOL 105, Summer 2012 Session II Page 215 of

12 1 minute essay - Summarize what you learned in this expedition - Avoid the "I learned a lot about" syndrome - show some insight I am here to help you learn the material. Remember that answer keys are not provided after exam #1, please do a selfassessment of your learning in this expedition and post any questions that you may have in the "Exped 19 Ocean & Climate - Any Questions" in the Desire2Learn Discussion area. In order to receive credit for completing this expedition, Go to Desire2Learn and send Bye Don End Expedition 19 in Subject Line. Include "Bye Don" in body of , Include Completion Word (see last page of expedition) and write your name in body of message General Oceanography, GEOL 105, Summer 2012 Session II Page 216 of

EARTH, PLANETARY, & SPACE SCIENCES 15 INTRODUCTION TO OCEANOGRAPHY. LABORATORY SESSION #6 Fall Ocean Circulation

EARTH, PLANETARY, & SPACE SCIENCES 15 INTRODUCTION TO OCEANOGRAPHY. LABORATORY SESSION #6 Fall Ocean Circulation EARTH, PLANETARY, & SPACE SCIENCES 15 INTRODUCTION TO OCEANOGRAPHY LABORATORY SESSION #6 Fall 2017 Ocean Circulation The focus of the Lab this week is circulation of the ocean and atmosphere. Here, you

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

Ocean Circulation. Si Hui Lee and Frances Wen. You can access ME at

Ocean Circulation. Si Hui Lee and Frances Wen. You can access ME at Ocean Circulation Si Hui Lee and Frances Wen You can access ME at http://tinyurl.com/oceancirculation Earth - the blue planet - 71% area covered by the oceans - 3/4 of ocean area between 3000-6000m deep

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

Currents & Gyres Notes

Currents & Gyres Notes Currents & Gyres Notes Current A river of water flowing in the ocean. 2 Types of Currents Surface Currents wind-driven currents that occur in the top 100m or less Deep Currents density-driven currents

More information

CHAPTER 7 Ocean Circulation

CHAPTER 7 Ocean Circulation 1 2 3 4 5 6 7 8 9 10 11 12 13 14 CHAPTER 7 Ocean Circulation Words Ocean currents Moving seawater Surface ocean currents Transfer heat from warmer to cooler areas Similar to pattern of major wind belts

More information

Ocean Layers. Based on sunlight penetration: Based on water density: Sunlight (photosynthesis is possible) Twilight Midnight

Ocean Layers. Based on sunlight penetration: Based on water density: Sunlight (photosynthesis is possible) Twilight Midnight PART 3 Ocean Layers Based on sunlight penetration: Sunlight (photosynthesis is possible) Twilight Midnight Based on water density: Mixed layer Pycnocline (rapid change of themperature/salinity) Deep ocean

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

170 points. 38 points In your textbook, read about modern oceanography. For each item write the word that meets the description.

170 points. 38 points In your textbook, read about modern oceanography. For each item write the word that meets the description. Ch 15 Earth s Oceans SECTION 15.1 An Overview of Oceans 38 points In your textbook, read about modern oceanography. For each item write the word that meets the description. (5 points) 1. German research

More information

Lecture 5.1 Surface Ocean Circulation. Image from Daily Mail Newspaper, UK

Lecture 5.1 Surface Ocean Circulation. Image from Daily Mail Newspaper, UK Lecture 5.1 Surface Ocean Circulation Image from Daily Mail Newspaper, UK Announcements Midterm is Thursday, consists of 25 multiple choice, 3 pages short answer questions No Scantron needed Calculators,

More information

The Ocean is a Geophysical Fluid Like the Atmosphere. The Physical Ocean. Yet Not Like the Atmosphere. ATS 760 Global Carbon Cycle The Physical Ocean

The Ocean is a Geophysical Fluid Like the Atmosphere. The Physical Ocean. Yet Not Like the Atmosphere. ATS 760 Global Carbon Cycle The Physical Ocean The Physical Ocean The Ocean is a Geophysical Fluid Like the Atmosphere Three real forces: Gravity Pressure gradients Friction Two apparent forces: Coriolis and Centrifugal Geostrophic & Hydrostatic balances

More information

Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all. interconnected as part of a single large global ocean.

Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all. interconnected as part of a single large global ocean. Ocean Motion Met 101: Introduction to the World's Oceans Produced by The COMET Program Geography: Name Pd. Earth s oceans covers 71 % _ of the planet s surface. In reality, Earth s ocean waters are all

More information

Role of the oceans in the climate system

Role of the oceans in the climate system Role of the oceans in the climate system heat exchange and transport hydrological cycle and air-sea exchange of moisture wind, currents, and upwelling gas exchange and carbon cycle Heat transport Two Primary

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

10% water in the world is tied up in the surface ocean currents. (above the pycnocline) Primary source is wind: Westerlies, Trades, Polar Easterlies

10% water in the world is tied up in the surface ocean currents. (above the pycnocline) Primary source is wind: Westerlies, Trades, Polar Easterlies Oceanography Chapter 9 10% water in the world is tied up in the surface ocean currents. (above the pycnocline) Primary source is wind: Westerlies, Trades, Polar Easterlies Coriolis deflects winds (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

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

Ocean Motion. Ocean Currents. Before You Read. Read to Learn

Ocean Motion. Ocean Currents. Before You Read. Read to Learn chapter 18 3 Ocean Motion section 2 Ocean Currents What You ll Learn the Coriolis effect what influences surface currents the temperature of coastal waters about density currents Before You Read Imagine

More information

and the Link between Oceans, Atmosphere, and Weather

and the Link between Oceans, Atmosphere, and Weather Geography Worksheet Instructions Using a map, atlas, or any other materials your teacher suggests, label the following on the blank map provided. 1. Label East, West, North, and South. 2. Label the following

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

Our Climate: A Global Challenge. Academy of Lifelong Learning Denver, CO April 9, 2015

Our Climate: A Global Challenge. Academy of Lifelong Learning Denver, CO April 9, 2015 Our Climate: A Global Challenge Academy of Lifelong Learning Denver, CO April 9, 2015 Oceans Thermohaline Circulation It takes water 500 to 1000 years to go around the planet. Thermohaline Circulation,

More information

9.3. Storing Thermal Energy. Transferring Thermal Energy

9.3. Storing Thermal Energy. Transferring Thermal Energy 9.3 If you have been to a beach on a hot summer day, you have likely cooled off by going for a dip in the water. The water, which is cooler than you are, removes thermal energy from your body, making you

More information

OCN 201, Chemistry & Physics Section

OCN 201, Chemistry & Physics Section , A 1-April-2015 Name: Answer the True/False and Multiple Choice questions on the scantron sheet. Answer the remaining questions on this exam handout. Turn in both the scantron and exam at the end of class.

More information

Agronomy 406 World Climates

Agronomy 406 World Climates Agronomy 406 World Climates January 30, 2018 Monsoons. Ocean properties and circulation. Review for today: Online textbook: 1.3.1 (Sea water) Composition and properties. For Thursday: Rahmstorf, S.: The

More information

Deep Water Currents Lab

Deep Water Currents Lab Deep Water Currents Lab Background: Anyone visiting the seashore is struck by the constant motion of water traveling on the surface of the ocean in the form of waves. But beneath the ocean's surface, water

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

OCN 201 Surface Circulation

OCN 201 Surface Circulation OCN 201 Surface Circulation Excess heat in equatorial regions requires redistribution toward the poles 1 In the Northern hemisphere, Coriolis force deflects movement to the right In the Southern hemisphere,

More information

(20 points) 1. ENSO is a coupled climate phenomenon in the tropical Pacific that has both regional and global impacts.

(20 points) 1. ENSO is a coupled climate phenomenon in the tropical Pacific that has both regional and global impacts. SIO 210 Problem Set 4 Answer key December 1, 2014 Due Dec. 12, 2014 (20 points) 1. ENSO is a coupled climate phenomenon in the tropical Pacific that has both regional and global impacts. (2 points) a)

More information

Greenhouse Effect Activity

Greenhouse Effect Activity Greenhouse Effect Activity Objectives: The student will: 1. Read and use weather instruments. 2. Collect and record temperature readings. 3. Describe the concept of the greenhouse effect. Materials: Fish

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

OCN201 Spring14 1. Name: Class: Date: True/False Indicate whether the statement is true or false.

OCN201 Spring14 1. Name: Class: Date: True/False Indicate whether the statement is true or false. Name: Class: _ Date: _ OCN201 Spring14 1 True/False Indicate whether the statement is true or false. 1. Short residence time elements are uniformly distributed in the oceans 2. Thermohaline circulation

More information

COASTAL UPWELLING - MONTEREY BAY CALIFORNIA (modified from The Maury Project, AMS)

COASTAL UPWELLING - MONTEREY BAY CALIFORNIA (modified from The Maury Project, AMS) Name: Date: Per: COASTAL UPWELLING - MONTEREY BAY CALIFORNIA (modified from The Maury Project, AMS) The ocean is composed of 3 distinct layers: the shallow surface mixed zone, the transition zone, and

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

Ocean Currents Unit (4 pts)

Ocean Currents Unit (4 pts) Name: Section: Ocean Currents Unit (Topic 9A-1) page 1 Ocean Currents Unit (4 pts) Ocean Currents An ocean current is like a river in the ocean: water is flowing traveling from place to place. Historically,

More information

Assessment Schedule 2016 Earth and Space Science: Demonstrate understanding of processes in the ocean system (91413)

Assessment Schedule 2016 Earth and Space Science: Demonstrate understanding of processes in the ocean system (91413) NCEA Level 3 Earth & Space Science (91413) 2016 page 1 of 6 Assessment Schedule 2016 Earth and Space Science: Demonstrate processes in the ocean system (91413) Evidence Statement Q Evidence with with Excellence

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

Chapter 22, Section 1 - Ocean Currents. Section Objectives

Chapter 22, Section 1 - Ocean Currents. Section Objectives Chapter 22, Section 1 - Ocean Currents Section Objectives Intro Surface Currents Factors Affecting Ocean Currents Global Wind Belts (you should draw and label a diagram of the global wind belts) The Coriolis

More information

Chapter 10. Thermohaline Circulation

Chapter 10. Thermohaline Circulation Chapter 10. Thermohaline Circulation Main References: Schloesser, F., R. Furue, J. P. McCreary, and A. Timmermann, 2012: Dynamics of the Atlantic meridional overturning circulation. Part 1: Buoyancy-forced

More information

SIO 210 Final examination Wednesday, December 11, PM Sumner auditorium Name:

SIO 210 Final examination Wednesday, December 11, PM Sumner auditorium Name: SIO 210 Final examination Wednesday, December 11, 2013 2-5 PM Sumner auditorium Name: Turn off all phones, ipods, etc. and put them away. This is a closed book exam. You may use one page of notes, both

More information

NOTE ->->-> DUE THURSDAY APRIL 20 TH 2006 THAT IS CORRECT I FORGOT THIS IS EASTER WEEKEND SO I HAVE EXTENDED THE DUE DATE TO THE ABOVE

NOTE ->->-> DUE THURSDAY APRIL 20 TH 2006 THAT IS CORRECT I FORGOT THIS IS EASTER WEEKEND SO I HAVE EXTENDED THE DUE DATE TO THE ABOVE GEO 130 NAME OCEANOGRAPHY TEST 3 TAKE HOME TEST SPRING 2006 NOTE ->->-> DUE THURSDAY APRIL 20 TH 2006 THAT IS CORRECT I FORGOT THIS IS EASTER WEEKEND SO I HAVE EXTENDED THE DUE DATE TO THE ABOVE This test

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

Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture!

Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction. Idealized 3-Cell Model of Wind Patterns on a Rotating Earth. Previous Lecture! Lecture 13 El Niño/La Niña Ocean-Atmosphere Interaction Previous Lecture! Global Winds General Circulation of winds at the surface and aloft Polar Jet Stream Subtropical Jet Stream Monsoons 1 2 Radiation

More information

IX. Upper Ocean Circulation

IX. Upper Ocean Circulation IX. Upper Ocean Circulation World Ocean Covers 71% of Earth s surface Contains 97% of surface water Arctic Ocean NH: 61% ocean, 39% land Pacific Ocean Atlantic Ocean Southern Ocean Indian Ocean SH: 81%

More information

The Surface Currents OCEA 101

The Surface Currents OCEA 101 The Surface Currents OCEA 101 Why should you care? - the surface ocean circulation controls the major ocean biomes - variations in ocean circulation control the supply of nutrients for marine organisms

More information

ATS150: Global Climate Change. Oceans and Climate. Icebergs. Scott Denning CSU 1

ATS150: Global Climate Change. Oceans and Climate. Icebergs. Scott Denning CSU 1 The Oceans Wind-Driven Gyre Circulations Icebergs Scott Denning CSU 1 Surface Balance of Forces friction coriolis wind stress resultant current Wind stress accelerates surface water Friction couples surface

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

Monday, October 2, Watch for new assessment (Week 4/5 review) TA s have your tests, please see key (at course website)

Monday, October 2, Watch for new assessment (Week 4/5 review) TA s have your tests, please see key (at course website) Monday, October 2, 2017 Watch for new assessment (Week 4/5 review) TA s have your tests, please see key (at course website) Homework 3 Due date Wednesday, Oct 11 (8 pm) Be ready to watch another important

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

ESS15 Lecture 12. Review, tropical oceans & El Nino, and the thermohaline ocean circulation. Please see new reading material on website.

ESS15 Lecture 12. Review, tropical oceans & El Nino, and the thermohaline ocean circulation. Please see new reading material on website. ESS15 Lecture 12 Review, tropical oceans & El Nino, and the thermohaline ocean circulation. Please see new reading material on website. Review. I-clicker exercise: In this graph of Earth s energy imbalances

More information

Zonal (East-West) Currents. Wind-Driven Ocean Currents. Zonal (East-West) Currents. Meridional (N-S) Currents

Zonal (East-West) Currents. Wind-Driven Ocean Currents. Zonal (East-West) Currents. Meridional (N-S) Currents Wind-Driven Ocean Currents Similarities between winds & surface currents Zonal (East-West) Currents Trade winds push currents westward north & south of the equator Equatorial currents. Up to 100 cm/sec.

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

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

Name: OBJECTIVES: By the end of today s lesson, you will be able to

Name: OBJECTIVES: By the end of today s lesson, you will be able to 7 th Grade Science Unit: Water s Cycles and Patterns Lesson: WCP 21 Name: Date: Monday, October 3, 2016 Homeroom: _ OBJECTIVES: By the end of today s lesson, you will be able to SWBAT Explain how currents

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 Circulation, Food Webs and Climate What does the wind have to do with feeding fish (and feeding us)?

Ocean Circulation, Food Webs and Climate What does the wind have to do with feeding fish (and feeding us)? Ocean Circulation, Food Webs and Climate What does the wind have to do with feeding fish (and feeding us)? El Niño: Tropical Oceans and Global Climate Reading: 9.10-9.13, 9.15 Graphic: Upwelling off Cape

More information

OCN-201 Chemistry and Physics section

OCN-201 Chemistry and Physics section Name: Class: _ Date: _ OCN-201 Chemistry and Physics section True/False Indicate whether the statement is true or false. 1. Because of the dissolved salt in seawater its freezing point is lower than that

More information

Lecture 13. Global Wind Patterns and the Oceans EOM

Lecture 13. Global Wind Patterns and the Oceans EOM Lecture 13. Global Wind Patterns and the Oceans EOM Global Wind Patterns and the Oceans Drag from wind exerts a force called wind stress on the ocean surface in the direction of the wind. The currents

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

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

OCEANOGRAPHY STUDY GUIDE

OCEANOGRAPHY STUDY GUIDE OCEANOGRAPHY STUDY GUIDE Chapter 2 Section 1 1. Most abundant salt in ocean. Sodium chloride; NaCl 2. Amount of Earth covered by Water 71% 3. Four oceans: What are they? Atlantic, Pacific, Arctic, Indian

More information

Directed Reading. Section: Ocean Currents. a(n). FACTORS THAT AFFECT SURFACE CURRENTS

Directed Reading. Section: Ocean Currents. a(n). FACTORS THAT AFFECT SURFACE CURRENTS Skills Worksheet Directed Reading Section: Ocean Currents 1. A horizontal movement of water in a well-defined pattern is called a(n). 2. What are two ways that oceanographers identify ocean currents? 3.

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

Oceans and the Global Environment: Lec 2 taking physics and chemistry outdoors. the flowing, waving ocean

Oceans and the Global Environment: Lec 2 taking physics and chemistry outdoors. the flowing, waving ocean Oceans and the Global Environment: Lec 2 taking physics and chemistry outdoors the flowing, waving ocean Peter Rhines 1 Eric Lindahl 2 Bob Koon 2, Julie Wright 3 www.ocean.washington.edu/courses/has221a-08

More information

from a decade of CCD temperature data

from a decade of CCD temperature data (Some of) What we have learned from a decade of CCD temperature data Craig Gelpi and Karen Norris Long Beach Aquarium of the Pacific August 15, 2008 Introduction Catalina Conservancy Divers collected temperature

More information

OCEANOGRAPHY 101. Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River.

OCEANOGRAPHY 101. Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River. OCEANOGRAPHY 101 EXAM 2 WINTER 00 NAME STUDENT NUMBER 1 Map, and temperature, salinity & density profiles of the water column at X, near mouth of the Columbia River. P a c i f i c O c e a n X WA Columbia

More information

SURFACE CURRENTS AND TIDES

SURFACE CURRENTS AND TIDES NAME SURFACE CURRENTS AND TIDES I. Origin of surface currents Surface currents arise due to the interaction of the prevailing wis a the ocean surface. Hence the surface wi pattern (Figure 1) plays a key

More information

Chapter 10 Lecture Outline. The Restless Oceans

Chapter 10 Lecture Outline. The Restless Oceans Chapter 10 Lecture Outline The Restless Oceans Focus Question 10.1 How does the Coriolis effect influence ocean currents? The Ocean s Surface Circulation Ocean currents Masses of water that flow from one

More information

Sailing the Seas: Wind Driven Ocean Circulation Ocean Gyres

Sailing the Seas: Wind Driven Ocean Circulation Ocean Gyres Sailing the Seas: Wind Driven Ocean Circulation Ocean Gyres Ocean Currents What Happens at the Coast? Readings: Ch 9: 9.2-9.6, 9.8-9.13 Graphic: America's Cup sailboat race off Newport, Rhode Island. J.

More information

Figure 8.8. Figure Oceanography 10 Ocean Circulation. Gulf Stream flows at 55 million cubic meters/sec, 500 times the flow of the Amazon River

Figure 8.8. Figure Oceanography 10 Ocean Circulation. Gulf Stream flows at 55 million cubic meters/sec, 500 times the flow of the Amazon River Oceanography 10 Ocean Circulation PART 1: Introduction General types of Ocean Currents Solar Energy and the Seasons PART 2: Measuring Ocean Currents and Structure PART 3: General Surface Currents and their

More information

Ocean Currents Shortcut method by to learn faster

Ocean Currents Shortcut method by to learn faster Ocean Currents Shortcut method by to learn faster In our geography notes on the hydrosphere, we have seen the major movements of the ocean water. They are waves, tides and ocean currents. Having covered

More information

Ocean Currents Shortcut method by to learn faster

Ocean Currents Shortcut method by to learn faster Ocean Currents Shortcut method by to learn faster In our geography notes on the hydrosphere, we have seen the major movements of the ocean water. They are waves, tides and ocean currents. Having covered

More information

Ocean Current Worksheet

Ocean Current Worksheet Ocean Current Worksheet Temperature Affects and Surface Currents: Surface waters of the Earth s oceans are forced to move, primarily by winds. Where winds blow in the same direction for a long period of

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

Water on Earth. How do oceans relate to weather and the atmosphere? Solar Radiation and Convection Currents

Water on Earth. How do oceans relate to weather and the atmosphere? Solar Radiation and Convection Currents Earth is often called the Blue Planet because so much of its surface (about 71%) is covered by water. Of all the water on Earth, about 96.5% is held in the world s oceans. As you can imagine, these oceans

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

Midterm Exam III November 25, 2:10

Midterm Exam III November 25, 2:10 Midterm Exam III November 25, 2:10 25, 2:10 3:25 pm, HW714 Chapters 7 (7.12 7.17), 8 and 9 (through section 9.15, included) 60 multiple choice questions this exam constitutes 22% (only) of your total (overall)

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

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

SIO 210 Introduction to Physical Oceanography Mid-term examination November 4, 2013; 50 minutes

SIO 210 Introduction to Physical Oceanography Mid-term examination November 4, 2013; 50 minutes SIO 210 Introduction to Physical Oceanography Mid-term examination November 4, 2013; 50 minutes Closed book; one sheet of your own notes is allowed. A calculator is allowed. (100 total points.) Possibly

More information

Level 3 Earth and Space Science, 2018

Level 3 Earth and Space Science, 2018 91413 914130 3SUPERVISOR S Level 3 Earth and Space Science, 2018 91413 Demonstrate understanding of processes in the ocean system 2.00 p.m. Thursday 22 November 2018 Credits: Four Achievement Achievement

More information

Quiz name: Oceanography - Land and Sea Interaction - Quiz #2

Quiz name: Oceanography - Land and Sea Interaction - Quiz #2 Name: Quiz name: Oceanography - Land and Sea Interaction - Quiz #2 ate: 1. What is the direction of spin for gyres in the northern hemisphere? clockwise counter clockwise northern oscillation southern

More information

Oceanography. Chapter 7 CIRCULATION PATTERNS AND OCEAN CURRENTS

Oceanography. Chapter 7 CIRCULATION PATTERNS AND OCEAN CURRENTS Oceanography Chapter 7 CIRCULATION PATTERNS AND OCEAN CURRENTS أ. راي د مرعي الخالدي Circulation Patterns and Ocean Currents 7.1 Density-Driven Driven Circulation 7.2 Thermohaline Circulation 7.3 The Layered

More information

Write about this. Have you ever experienced a very strong wind gust? What happened? Have you ever felt a gentle breeze? What did it feel like?

Write about this. Have you ever experienced a very strong wind gust? What happened? Have you ever felt a gentle breeze? What did it feel like? Write about this. Have you ever experienced a very strong wind gust? What happened? Have you ever felt a gentle breeze? What did it feel like? How wind works Winds flow on earth based on differences in

More information

OCN 201 Lab Fall 2009 OCN 201. Lab 9 - El Niño

OCN 201 Lab Fall 2009 OCN 201. Lab 9 - El Niño OCN 201 Lab Fall 2009 OCN 201 Lab 9 - El Niño El Niño is probably one of the most widely publicized oceanic phenomena. If there s one single reason for that it s probably the fact that El Niño s presence

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

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

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

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

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

Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams

Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams Summary of Lecture 10, 04 March 2008 Introduce the Hadley circulation and examine global weather patterns. Discuss jet stream dynamics jet streams arise because the Coriolis force prevents Hadley-type

More information

- terminology. Further Reading: Chapter 07 of the text book. Outline. - characteristics of ENSO. -impacts

- terminology. Further Reading: Chapter 07 of the text book. Outline. - characteristics of ENSO. -impacts (1 of 14) Further Reading: Chapter 07 of the text book Outline - terminology - characteristics of ENSO -impacts (2 of 14) Today: Introduction We want to look at another source of variability in the atmosphere

More information

surface salinities temperature profiles of the ocean; the thermocline seawater density dynamics deep ocean pressures

surface salinities temperature profiles of the ocean; the thermocline seawater density dynamics deep ocean pressures NATURE OF SEAWATER: SALINITY, TEMPERATURE, DENSITY, AND PRESSURE surface salinities temperature profiles of the ocean; the thermocline seawater density dynamics deep ocean pressures Part A. Surface Salinities

More information

SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011

SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011 SIO 210 Problem Set 3 November 4, 2011 Due Nov. 14, 2011 1. At 20 N, both the ocean and the atmosphere carry approximately 2 PW of heat poleward, for a total of about 4 PW (see figure). If (at this latitude)

More information

What is an ocean current? 1. wind action: the force of the wind blowing over the top of the water 2. spin of Earth 3. shape of the continents

What is an ocean current? 1. wind action: the force of the wind blowing over the top of the water 2. spin of Earth 3. shape of the continents Ocean Currents Textbook pages 414 427 Before You Read Section 11.2 Summary What forces do you think cause ocean water to move? Do you think ocean water moves the same way everywhere in the ocean? Write

More information

The Air-Sea Interaction. Masanori Konda Kyoto University

The Air-Sea Interaction. Masanori Konda Kyoto University 2 The Air-Sea Interaction Masanori Konda Kyoto University 2.1 Feedback between Ocean and Atmosphere Heat and momentum exchange between the ocean and atmosphere Atmospheric circulation Condensation heat

More information

Current: large mass of continuously moving ocean water

Current: large mass of continuously moving ocean water Ocean Currents Current: large mass of continuously moving ocean water Surface Currents--Wind Circulation These waters make up about 10% of all the water in the ocean. These waters are the upper 400 meters

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

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

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

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