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Lesson Six: Surface Currents Which factors in the earth system create gyres? Why does collect in the gyres?

Objective: Develop a model that shows how patterns in atmospheric and ocean currents create gyres, and explain why collects in them. Introduction: Gyres are circular, wind-driven ocean currents. Look at this map of the five main subtropical gyres, where the colors illustrate enormous areas of floating waste. These are places in the ocean that accumulate floating debris—in particular, plastic pollution.

How do you think ocean gyres form? What patterns do you notice in terms of where the gyres are located in the ocean?

The Earth is a system: a group of parts (or components) that all work together. The components of a system have different structures and functions, but if you take a component away, the system is affected. The system of the Earth is made up of four main subsystems: hydrosphere (water), (air), geosphere (land), and biosphere (organisms). The ocean is part of our planet’s hydrosphere, but it is also its own system.

Which components of the Earth system do you think create gyres, and why would pollution collect in them?

Activity 1 Gyre Model: How do you think patterns in ocean currents create gyres and cause pollution to collect in the gyres? Use labels and arrows to answer this question. Keep your diagram very basic; we will explore this question more in depth as we go through each part of the lesson and you will be able to revise it.

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Activity 2 How Do Gyres Form?

A gyre is a circulating system of ocean boundary currents powered by the uneven heating of air masses and the shape of the Earth’s coastlines. These gyres occur north and south of the . There are five main gyres where trash accumulates in the ocean: The , The , The , The , and The Indian Oceanic Gyre.

An is a river of water moving in the ocean; they can be at the surface, as well as deep in the ocean. Surface ocean currents are called convection currents; they form due to differences in . Surface ocean currents move as wind drags on the ocean’s surface. The water moves and builds up in the direction that the wind is blowing.

Differences in air temperature cause wind. Air masses move from areas of high pressure toward areas of low pressure. In general, air masses are colder at the poles and have higher density (high pressure) than air at the equator, which is warmer and has a lower density (low pressure). These differences in temperature and pressure cause colder air masses to move toward the equator, while warmer air masses move from the equator toward the poles.

If the Earth remained still, the atmosphere would only circulate between the poles and the equator. However, the Earth spins on its axis, resulting in the Coriolis Effect, which describes the ground moving at a different speed than an object in the air. The Earth makes a complete rotation about its axis approximately once every 24 hours, and has a greater circumference at the equator than at the poles—so it spins faster at the equator than at the poles. As the Earth spins, it causes the earth’s air masses to curve toward the right in the (in a clockwise motion) and to curve toward the left in the Southern Hemisphere (in a counterclockwise motion). This sets up global wind patterns that circulate air masses around the Earth and influence surface ocean currents. The air masses pull on the surface ocean water and drag it in the direction that the air is moving. This combination of factors create the gyres.

Use what you learned from this reading to revise your Activity 1 model (page 2).

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Activity 3 Modeling The Coriolis Effect: What effect might the Earth’s spinning have on the way air and water move? Model a fluid (either water or air) traveling across the Earth. Materials

• Round fruit with a peel and without a stem, such as an orange or melon* • A globe or world map • Dry erase markers, in different colors

Directions 1. Form into partners or groups. 2. Refer to the map, and use the dry erase to mark: a. Arctic Circle and North Pole b. Antarctica and the South Pole c. Equator 3. One student holds the fruit still, while another marks a line from the North Pole to the Equator.

Observe what happens as the line is drawn from the colder area of high pressure to the warmer area of lower pressure. How does the line appear to move?

4. The student holding the fruit slowly turns it in a circle from left to right, while a second line is drawn from the North Pole to the Equator, using a different colored marker. Watch the line from the perspective of the North Pole.

What happened to the line?

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5. One student holds the fruit still, while another marks a line from the South Pole to the Equator, using another colored marker.

Observe what happens as the line is drawn from the warmer area of high pressure to the colder area of lower pressure. How does the line appear to move?

6. The student holding the fruit slowly turns it in a circle from left to right, while a second line is drawn from the South Pole to the Equator, using a different colored marker. Watch the line from the perspective of the South Pole.

What happened to the line?

What pattern do you see among all of your data?

Optional: Watch “Surface Ocean Currents” video to learn more.

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Activity 4 Modeling Ocean Currents: Develop and use a model to describe how unequal heating, the rotation of the earth, and land boundaries causes patterns of oceanic circulation that create gyres in the ocean system.

Carefully review this thermal map of the Earth. What pattern do you see in the earth’s temperature? Which zones of the earth are the warmest? The coldest?

We will explore how the different of the earth affect the ocean by conducting an investigation using an ice cube and water. What happens when different temperatures of water come in contact with each other? What do you think will happen when you place the ice cube in the cup of room temperature water?

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Materials

• Ice cube • Clear glass filled with warm water • Liquid food coloring

Directions 1. Place the ice cube in the water. 2. After one minute, add a drop of food coloring to the top of the ice cube.

Observe the glass. Which direction is the colored water moving? Moving water within another body of water is called a current. Is this what you have created in the glass? Draw and describe your model below.

One characteristic that we use to describe matter is its density. Density is the amount of matter in a given volume of an object. When we compare the density of one piece of matter to another, we generally use the idea of heaviness. Objects that are denser than their surroundings tend to sink, while objects that are less dense than their surroundings tend to float. In denser objects, molecules tend to be closer together, while a less dense object’s molecules tend to be further apart.

Did the ice cube float or sink when it was placed in the water? Based on your response, how would you expect the molecules to look inside the ice cube, as compared to the room temperature water—would they be closer together or farther apart?

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Temperature affects the density of a substance. Temperature measures the kinetic energy or movement of molecules within a substance. Would you expect molecules to move faster or slower at higher temperatures? Would a substance at a higher temperature be denser or less dense than at a lower temperature?

We would expect ice to be denser than liquid water because it has a lower temperature. The density of ice is unique because it does not follow this general rule. Water molecules contain a type of bonding, called bonding. The hydrogen bonds hold water molecules slightly farther apart from one another as solid ice forms, in what is known as a crystal lattice formation. This is why ice is less dense than water. It is a good thing too because life as we know it would not exist if ice did not float. The thin layer of ice that floats atop many lakes and bodies of water during winter provides warmth for the organisms that live in the water and is an important part of maintaining our .

Ice melt is fresh water that melts from a block of ice in the ocean. We demonstrated this in your experiment by placing a block of ice into room temperature water. What happens to the temperature of ice melt as it interacts with room temperature water? Use evidence from your experiment to explain your reasoning.

Which was denser, the ice melt or room temperature water? Use evidence from your experiment to explain your reasoning.

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A current should have formed in the cup as the ice melted. Describe both the temperature and density of water molecules that you would expect to sink versus those that expected to rise.

Think about the thermal map of the Earth and the experiment of the ice being placed in the glass of water. What does the cup, ice and water represent in an Earth system?

How does this system help us to understand what happens in the ocean when different temperatures of water come into contact with each other?

How does the system help us to understand what happens when plastic pollution becomes part of this system?

Use your recent experience to revise your Activity 1 model (page 2). Show changes in the temperature and density of water molecules as the ice melts. Be sure to include the role of temperature and density in how a gyre forms. Remember to include labels and use arrows to show any type of movement on your model.

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Activity 5 Spill Spread: How do uneven heating, the Coriolis Effect, and the shape of coastlines affect how pollution is transported through the ocean? Explore how currents spread pollution by creating a model of the ocean system.

Review notes from previous activities. What components of the Earth system will we need?

Materials

• 7 rocks • Container large enough to fit the rocks without touching • Water • Liquid food coloring in five colors • Ice cube

Directions 1. Place rocks in the water without touching in a formation that represents the continents. 2. Pour water over the container until the rocks are halfway submerge.

Diagram your system and label the parts.

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Prediction: What will happen to the pollution (food coloring) when it is added to the ocean (water) and why?

3. Add the ice cube at the top of the model. 4. Squeeze a few drops of different-colored food coloring into the water in areas representing the North Pacific Gyre, the South Pacific Gyre, the North Atlantic Gyre, the South Atlantic Gyre, and the . What types of pollution could be represented by the food coloring?

As the ice melts, what happens to your model? What can you see? What factors might affect your model that you cannot see?

How did the continents affect the spread of pollution?

How does your model help to explain how pollution ends up in the 5 Gyres?

5. Return to your diagram and add the new information that you learned from the experiment about how gyres from and trap pollution, especially plastic, in the ocean.

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Lesson Five: Ocean Currents Educator Facilitation Notes NGSS Standards

• SEP: Carry out an investigation; develop and use models • PE: MS-Ess2-4. Develop and use a model to describe how unequal heating and rotation of the Earth cause patterns of atmospheric and oceanic circulation that determine regional climates. • DCI: ESS3.C. The Roles of Water in Earth’s Surface Processes • DCI: ESS3.C. Weather and Climate • CCC: Patterns, systems and system models, cause and effect

Vocabulary

• Gyre • Hydrosphere • Atmosphere • Geosphere • Biosphere • Density • Coriolis effect • Density • Kinetic energy • Ice melt • Ocean current • Convection current Materials

• Round fruit with a peel and without a stem, such as an orange or melon • A globe or world map • Dry erase markers, in different colors • Ice cube • Clear glass filled with warm water • Liquid food coloring

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Timeline: Four 50-minute Activity Blocks 20 minutes Intro + Activity 1: Gyre Model 10 minutes Activity 2: How Do Gyres Form? 30 minutes Activity 3: Modeling the Coriolis Effect 50 minutes Activity 4: Modeling Ocean Currents 50 minutes Activity 5: Spill Spread

Activity Answer Key

What patterns do you notice in terms of where the gyres are located in the ocean? They occur next to or between continents; they all have a similar shape; they occur in different ; there are none at the equator or the poles.

What happens to the temperature of ice melt as it interacts with room temperature water? The cold water moved down toward the bottom of the cup and the warm water moved up toward the top of the cup, creating a convection current. Think about the thermal map of the Earth and the experiment of the ice being placed in the glass of water. What does the cup, ice and water represent in an Earth system? The cup represents the Earth, the room temperature water represents water at the equator, and the ice cube represents water at the poles. How did the cup represent and not represent the Earth? It represents the Earth in that it held the water and system, and had air and water in it; it did not represent the Earth in that there was no land, animals, people or plants on it. Why didn’t the ice cube sink when placed in the water; how would you expect the molecules to look inside the ice cube as compared to the room temperature water? The ice cute is less dense than the room temperature water; the molecules would be futher apart because the ice cube is less dense. Would you expect molecules to move faster or slower at higher temperatures? Would a substance at a higher temperature be denser or less dense than at a lower temperature? Molecules would move faster at a higher temperature and be less dense because the molecules are more spread out.

As the ice melts, what happens to your model? What can you see? What factors might affect your model that you cannot see? The factors that you can see are particles moving and convection currents; factors that you cannot see include temperature.

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What types of pollution could be represented by the food coloring? Runoff from streets and storm drains, agricultural waste, illegal dumping directly into the ocean, etc. Coriolis Effect Modeling Activity Notes

• The activity can be done with a real globe or printed picture of a map instead of a fruit; in that case, one student will need to rotate the paper slowly while the other attempts to slowly draw a straight line from pole to pole. • As the students draw lines on the “globe,” it should appear to curve toward the right (clockwise) in the northern hemisphere and toward the left (counterclockwise) in the southern hemisphere. Ocean Current Modeling Activity Notes

• The ice cube should float when placed in the water. • This activity can repeated to simulate thermohaline currents, which form differences in density and temperature due to a concentration of salt in ocean water, surrounding temperatures, and gravity. To demonstrate this phenomenon, repeat the experience with a salt water solution. Source Material Modeling the Coriolis Effect www.carolina.com/teacher-resources Ocean Currents Teacher’s Guide, published by Lawrence Hall of Science Great in Math and Science (GEMS) NOAA’s National Ocean Service Education: Currents National Oceanic and Atmospheric Administration, http://oceanservice.noaa.gov/education/kits/currents

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Sample Model

Thank you to Costa and ASPIRE schools for supporting the development of this curriculum.

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