Adrift A Classroom Activity for Ocean Gazing Episode 18: The princeʼs predictions: Part II

Similar documents
Position and displacement

Where are you right now? How fast are you moving? To answer these questions precisely, you

Lesson one. Linear Motion. Terminal Objective. Lesson 1. Linear Motion

MARCOOS CONFERENCE CALL FRIDAY, July 25, 2008 *All meetings are tape recorded*

HONORS PHYSICS One Dimensional Kinematics

Spirit Lesson 3 Robot Wheelies Lesson Outline Content: Context: Activity Description:

(Lab Interface BLM) Acceleration

In this lesson, students determine the speed of a tsunami using tsunami time travel maps and Google Earth.

Surf Clams: Latitude & Growth

L E S S O N : Tsunami Simulation Experiment

What s UP in the. Pacific Ocean? Learning Objectives

UNDERSTANDING STORM SURGE

SURFACE CURRENTS AND TIDES

Section 1. Objectives:

Riverboat Simulator Activity

Modeling Beach Erosion

Black Sea Bass Encounter

Chapter 11 Motion. Section 1

OIMB GK12 CURRICULUM

Standard 3.1 The student will plan and conduct investigations in which

Engineering Design Challenge. Mapping the Ocean Floor

Discussion Session 3 2D Relative Motion Week 04

Catch The SEACOOS Wave!

Pattern-Block Fish. Pat and Sam were having fun building fish with pattern blocks. 1 fish had 2 fins. 2 fish had 4 fins. 3 fish had 6 fins.

5. The magnitude of a vector cannot be smaller than the magnitude of any of its components. TRUE FALSE

The Hudson s Ups and Downs

Activity: Because the Earth Turns

Growth: Humans & Surf Clams

GLOBE Data Explorations

Riverboat Simulator Activity Sheet

Chartwork Learn the basics for position fixing using a number of techniques and a simple equation for speed, distance and time.

Grade: 8. Author(s): Hope Phillips

F I N D I N G K A T A H D I N :

Scales of Atmospheric Motion Scale Length Scale (m) Time Scale (sec) Systems/Importance Molecular (neglected)

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

SCI-5 MES_Lamb_Oceans Exam not valid for Paper Pencil Test Sessions

Beach Profiles: Monitoring Sea Level Rise. Student Activity Sheet. Name Date Class

1. A rabbit can cover a distance of 80 m in 5 s. What is the speed of the rabbit?

Unit 1 Uniform Velocity & Position-Time Graphs

Chapter 11 Motion. Displacement-. Always includes Shorter than distance

2 Characteristics of Waves

Due Next Class: U1.HW1.Dist/Disp & P-t Graphs All (problems 1-3) Do Now: 1. Walk in silently.

Measuring Flow with. Centre County PaSEC. QC Team July P a g e

CBIBS 2008 Online Data Scavenger Hunt by Christopher Petrone; Adapted from CBIBS 2007 Data Scavenger Hunt by Lorraine Brasseur

GEOG2113: Geographical Information Systems Week 7 Mapping Hazards & Threats Practical Task

2 Motion BIGIDEA Write the Big Idea for this chapter.

Unit 3 ~ Learning Guide Name:

The speed of an inline skater is usually described in meters per second. The speed of a car is usually described in kilometers per hour.

Remeber this? You still need to know this!!!

Vocabulary: Objectives: Materials: For Each Station: (Have 2 stations for each liquid; 8 stations total, in student groups of 3-4) Students will:

Physics 11 Honours Lesson 3 Distance and Displacement

LAB : Using A Spark Timer

Ocean Currents Lecture Notes

GRADE 9: Physical processes 3. UNIT 9P.3 12 hours. Waves. Resources. About this unit. Previous learning. Expectations

Comparison of Wind Measurements at Nuchek Heights, Hinchinbrook Island, and at Seal Rocks NOAA Data Buoy in Hinchinbrook Entrance, Alaska

Lab 5: Ocean Waves and Tides

STUDENT PACKET # 10. Vocabulary: condensation, convection, convection current, land breeze, sea breeze

Well, Well, Well. BACKGROUND Seasonal upwelling is a very important process in the coastal ocean of the Pacific Northwest.

1.6.1 Inertial Reference Frames

Observing Waves, Their Properties, and Relationships

Buoyancy and Density. Buoyant Force and Fluid Pressure. Key Concept Buoyant force and density affect whether an object will float or sink in a fluid.

OIMB GK12 CURRICULUM. Beach Hopper Introduction and Jumping Experiment

Your web browser (Safari 7) is out of date. For more security, comfort and. the best experience on this site: Update your browser Ignore

A Pyramid of Crunchkins

Synthesis of marine debris modeling and observations: recent progress in understanding and applications

Note! In this lab when you measure, round all measurements to the nearest meter!

Green crabs: invaders in the Great Marsh Featured scientist: Alyssa Novak from the Center for Coastal Studies/Boston University

Guide to Providing Shoreside and Underway Training Opportunities to Sea Cadets & Sea Scouts

Two-Dimensional Motion and Vectors

Gears Ratios and Speed / Problem Solving

Lesson 2: Sailing. A league is three nautical miles. (A nautical mile is about 800 feet longer than a mile on land.)

Investigating Factors That Affect Tsunami Inundation A Science Inquiry

Temperature, salinity, density, and the oceanic pressure field

reported in stream flow.

The Aral Sea

Palythoa Abundance and Coverage in Relation to Depth

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

Student Exploration: Ripple Tank

Our Council s Own: Oceanography Cadette/Senior/Ambassador Badge

SOCCOM.Act.PDS.1.1: Tracking Ocean Currents

Unit 11 Lesson 2 How Does Ocean Water Move? Copyright Houghton Mifflin Harcourt Publishing Company

Physical Science You will need a calculator today!!

Name: Class: Date: Multiple Choice Identify the letter of the choice that best completes the statement or answers the question.

100-Meter Dash Olympic Winning Times: Will Women Be As Fast As Men?

Shedding Light on Motion Episode 4: Graphing Motion

AP Physics B Summer Homework (Show work)

Contents DE LA SALLE COLLEGE OLLIE USAGE GUIDE 2

SEASONDE DETECTION OF TSUNAMI WAVES

Vocabulary. Page 1. Distance. Displacement. Position. Average Speed. Average Velocity. Instantaneous Speed. Acceleration

and the Link between Oceans, Atmosphere, and Weather

Investigating the Speed of Earthquake Waves

Slide 1 - Welcome to an Overview of the Student Center and New Titan Online

Activity Overview. Granny on the Ramp: Exploring Forces and Motion MO-BILITY. Activity 4B MS. Activity Objectives: Activity Description:

Do Now 10 Minutes Topic Speed and Velocity

Gravity: How fast do objects fall? Teacher Version (Grade level: 4 7)

114 The Oregon Coast Book, Edition. Check website for updates: hmsc.oregonstate.edu/quests

Parametric Ball Toss TEACHER NOTES MATH NSPIRED. Math Objectives. Vocabulary. About the Lesson. TI-Nspire Navigator System

Vanishing Coast: Erosion

Introduction to solving acceleration problems

LESSON 2: SUBMARINE BUOYANCY INVESTIGATION

Transcription:

Adrift A Classroom Activity for Ocean Gazing Episode 18: The princeʼs predictions: Part II Written by: Liesl Hotaling (CIESE at Stevens Institute of Technology), Daniel Griesbach (Homdel High School), Paul Ludgate (Upper Township Middle School), Janice McDonnell and Eric Simms (IMCS-Rutgers University) Edited by: Amy Pallant and Debra Kovacs (Turnstone Publishing) Reviewed by: Michael Crowley, Dr. Scott Glenn, Dr. Josh Kohut, and Sage Lichtenwalner (IMCS-Rutgers University) Supported by: The National Ocean Partnership Program Grade Level: 7-8 Lesson Time: Three to four 45-50 minute sessions Summary In this lesson cluster, students will work with component and resultant vectors. They will learn that the motion of an object is a function of many different forces. Students will then graphically add vectors to determine the displacement of a boat adrift at sea. Through this task, the concepts of distance and displacement will be distinguished. Ultimately, students will use real-time CODAR data for sea surface currents to determine the drift rate of a ship in the ocean and predict its eventual location. Predictions will be compared in following days to the actual sea surface current data to assess the validity of the students hypotheses. Objectives ü Step #1: Learn the Tools Understanding Ocean Currents and CODAR. Students visit the Control Room and background material what Coastal Ocean Radar (CODAR) is and how it works. ü Step #2: Analyze Data Practice Analyzing CODAR Images. Students will understand how surface currents are mapped and how to analyze data contained on the maps. ü Step #3: Pracitce Calculations Adding Vectors. Students will use both component and resultant vectors to solve a problem and understand the concept of vector addition ü Step #4 and #5: Using Real-Time CODAR Data to Locate the Ship. Students will use real-time CODAR data for sea surface currents to determine the drift rate of a ship in the ocean and predict its eventual location Introduction Navigation and ocean currents If you have ever dropped something in the ocean, you have probably seen how the ocean tends to carry it away from you, and you ve watched it bob up and down in waves. The movement of the object you ve

seen is caused by the influence of the ocean s surface currents and waves on the object. Boats on the ocean are able to travel with, or against, the currents on the ocean s surface by using oars, sails, or motors. However, if a boat loses its ability to move across the water, or is overcome by a storm, it will quickly find itself at the mercy of the wind, waves and currents. When boaters find themselves in trouble, they rely on the U.S. Coast Guard s Search and Rescue Unit to respond to their distress calls. If the Coast Guard knows how the surface currents are moving, they can locate boats and people more quickly. But how can ocean scientists (and the Coast Guard) see how the currents on the surface of the ocean are moving? In this project, you will learn how to read vector images of real-time CODAR (Costal Ocean Radar) data. Then you ll use your knowledge to help locate a lost ship off the New Jersey coast! Step 1: Learn the Tools; Understanding Ocean Currents and Coastal Ocean Radar (CODAR) Learn about CODAR. Visit the CODAR page in the What s COOL? section to learn how CODAR is used to study ocean surface currents and conditions. Then use the Control Room CODAR tutorial and the CODAR Science Background to explore component and resultant vectors of motion and to learn for yourself how surface currents are measured. When you re done close the windows to continue with this project. 1. Read about CODAR in What s COOL. 2. Go to the Control Room and click on the CODAR lever to do the CODAR tutorial. Based on what you ve learned about CODAR, answer the following questions. Record the answers on the Adrift Activity 1. Download the Adrift Activity 2. Make a list of the different forces you think would affect the motion of a drifting boat under Understanding Ocean Currents and CODAR. 3. Do you think it would be easy to determine the eventual motion of a drifting boat using all the forces you have listed so far? Why or why not? 4. Record your answers to the questions on the Adrift Activity Step 2: Analyze Data; Practice Analyzing CODAR Images Now let s apply your knowledge of vectors to some real CODAR images. In the following image, the CODAR system has produced a vector indicating the direction and speed of the surface current. The arrow you see is the combined, or resultant, motion for all the forces acting on the water at that point. 1. Examine the vectors. 2. Refer to the the Adrift Activity Worksheet to answers the questions Adrift Page 2

under Practice Analyzing CODAR Images. 3. Determine the current velocity (cm/sec) using the color scale on the right of the graph. 4. Use the COOLroom Speed Conversion calculator to convert the velocity to km/hour. To get there, scroll down to the middle of the COOLroom s Ocean Surface Currents from Coastal Radars page. Close the window when done. 5. Use the map scale (km) to determine the distance between the starting point (the non-arrowed end) of the vector and the point on land reached by drawing a straight line from the vector (in the direction it is pointing) until you hit land. Use the following formula to determine how long it would take for a wave starting at the vector to reach shore. If you know that Distance = Rate (or velocity) x Time, you can rearrange the equation as: Time = Distance/Rate (or velocity) Be sure to record your answers on the Adrift Activity Step 3: Practice Calculations; Adding Vectors Imagine that a group of middle school students is taking a field trip aboard a research vessel off the coast of New Jersey. The vessel is caught in a sudden storm and the engine breaks down, leaving the students adrift at sea for three days before the Coast Guard can rescue them (don t worry they have plenty of food!). The last known location of the vessel is 10 miles East of Ocean City, NJ. Record all your answers on the Adrift Activity Worksheet under Adding Vectors. The location of the boat is indicated on the map by a red dot approximately 10 miles off shore. 1. Look at the vector for Day 1. To determine how far the boat drifted in the first 24 hours, measure the length of the vector for Day 1 in centimeters (cm). Use the conversion of 1 cm = 21.4 cm/sec and convert to km/hr using the C.O.O.L. Room Speed Conversion calculator. Then multiply your answer by 24 hours to obtain the distance traveled on Day 1. Repeat the calculations for the vectors for Days 2 and 3. 2. Draw a straight line connecting the starting point on Day 1 to the ending point on Day 3. This line is the resultant vector. Measure the length of the vector in cm, and then use the scale 1 cm = 18.5 km to calculate the distance between the two points. Analysis: Answer the following questions on the Adrift Activity Worksheet under Adding Vectors. Adrift Page 3

1. Add the component vectors from each of the three days to determine the total distance the boat drifted. 2. How far from the starting point was the boat eventually located? How does this differ from adding the component vectors over the three days? Step 4: Use Real-Time CODAR Data; Coast Guard Search As a member of the Coast Guard Search and Rescue Unit, you have just received a distress call from a ship stranded at sea. You will now need to apply your knowledge of vectors, surface currents and the interaction of forces on ocean water to predict the expected location of the ship. You will do this by calculating the time it will take for the ship to reach a specified end point from a known starting point in the ocean. Record all of your answers on the Adrift Activity Worksheet under Using Real-Time CODAR Data. 1. Examine real-time data: a. Go the Boaters section of the COOLroom at http://www.thecoolroom.org/boa ters.htm and click on the link Ocean Surface Currents from CODAR. b. Scroll down the page to the second map, which shows the area of the ocean off the coast of New Jersey from Brant Beach to Brigantine. The small blue square at the top of the map is the Brant Beach CODAR station, and the blue square further south along the coast is the CODAR station at Brigantine. c. Print the image. d. Discuss any differences between this map and the ones used in the previous activities. 2. Discuss the overall trends and patterns observed for this day: a. What is the general direction of the surface currents? b. What is the fastest current speed on the map? c. What is the slowest current speed on the map? d. In what direction would a bottle drift if you dropped it at latitude 39:25 and longitude 74:05? Step 5: Predict Motion; Locate the Ship 1. Using latitude and longitude coordinates provided by the teacher, find the vector to be used as the starting point where the ship first sent a distress call. Based on the color of the vector, determine the speed (km/hour) of the surface currents at this location by comparing the color to the velocity scale to the right of the map. 2. Use the map scale (km) to determine the distance between the starting point (the non-arrowed end) of the selected vector and the selected end point. The end point is determined by drawing a straight line from the vector (in the direction it is pointing) until you hit land, or you reach the edge of the map (if the vector is pointing away from land). 3. Use the formula Time = Distance x Rate (or velocity), calculate the amount of time it would take for the ship to reach the selected end point. Do you predict that the ship will travel in a straight line to the end point? If not, why? Think back to the beginning of the unit when you hypothesized about the forces that would affect the motion of a drifting boat. Was the speed and direction of Adrift Page 4

the wind one of your factors? You may wish to check the real-time wind speed and direction of the wind from the Meteorological Tower at the Rutgers Marine Field Station (http://www.thecoolroom.org/boate rs/boat_met.htm) to see how the wind might affect the movement of the currents. 4. Check the real-time CODAR data over the next two-three days (or for as long as the amount of time you calculated in Step 5). Answer the corresponding question on the Adrift Activity Sheet. Sources To access an online version of this activity, you can go to the following URL: http://coolclassroom.org/cool_projects/les sons/physics_middleschool/locatetheship. html The related podcast episode for this activity can be found by going to the podcast section of www.oceangazing.org Adrift Page 5