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Laabri

2.09 Deep Ocean Circulation Lab

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Learning Objectives

  • Explain how ocean currents move water around the globe, including where water sinks, travels deep underwater, and rises back to the surface

  • Describe the effect of rising temperatures and melting sea ice has on deep ocean currents

Success Criteria

  • Identify and describe the major parts of the ocean conveyor belt

  • Explain the relationship between density, salinity, and temperature has on ocean movement

If you need help, click here to watch the recording

Learning Objectives

  • Explain how ocean currents move water around the globe, including where water sinks, travels deep underwater, and rises back to the surface

  • Describe the effect of rising temperatures and melting sea ice has on deep ocean currents

Success Criteria

  • Identify and describe the major parts of the ocean conveyor belt

  • Explain the relationship between density, salinity, and temperature has on ocean movement

If you need help, click here to watch the recording

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1.

Thinking back to the Surface Currents Lab, what powers the ocean's surface currents?

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2.

We're going to be mentioning the "Arctic" and "Antarctic" a lot, so let's make sure we know what that means. The images on the left have some fun facts about each area.

Arctic refers to the

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3.

Review: Think about what we learned in the Seawater Lab

In areas of the ocean where water sinks, the sinking water would have these characteristics:

  • Density:

  • Salinity: and the heat lamp represents the

The combination of cold temperatures and extra salt powers the Great Ocean Conveyor Belt, a massive, slow-moving, interconnected system of ocean currents that circulates water, nutrients, and heat around the entire globe.

This is also known as thermohaline circulation. Thermo = heat, haline = salt

Let's imagine we could hop a ride on the Global Ocean Conveyor Belt and hit all of the major stops.

Let's start in the North Atlantic

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8.

Video no longer available :(

Question 9
00:47
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9.

The cold, salty, dense water from the North Atlantic flows of the ocean towards the equator.

Question 10
00:56
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10.

The cold, salty, dense water continues south towards Antarctica.

Why don't deep ocean currents rise to the surface at the Equator?

Question 11
01:04
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11.

In the Southern Ocean surrounding Antarctica, the deep ocean current would become .

As a result, the deep ocean current water

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13.

Select the areas of upwelling (where deep ocean water rises to the surface)

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14.

Now that we have traveled through the Global Ocean Conveyor Belt, let's summarize the major parts by matching the description to the appropriate image.

Draggable itemarrow_right_altCorresponding Item

The current is "recharged" as it travels along the coast of Antarctica and picks up more cold, salty, dense water.

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The now-warmed surface waters continue circulating around the globe. They eventually return to the North Atlantic where the cycle begins again.

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Cold, salty, dense water sinks at the Earth's northern polar region and heads south along the western Atlantic basin.

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The main current splits into two sections, one traveling northward into the Indian Ocean, while the other heads up into the western Pacific.

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The two branches of the current warm and rise as they travel northward, then loop back around southward and westward.

arrow_right_alt

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15.

Below is a model of the Northern Atlantic Ocean.

Identify the location where water becomes very dense due to low temperature and high salt concentration.

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16.

Predict: What would happen if temperature rose and less sea ice formed?

Question 17
01:49
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Question 18
02:06
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Question 19
03:59
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20.
Mmuae Afoforo a Wobɛpaw:

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21.

The model represents that deep ocean circulation would density near the Arctic.

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22.

Reflect on your understanding of the learning objectives:

Explain how ocean currents move water around the globe, including where water sinks, travels deep underwater, and rises back to the surface

Describe the effect of rising temperatures and melting sea ice has on deep ocean currents

Reflect on your mastery of the success criteria:

Identify and describe the major parts of the ocean conveyor belt

Explain the relationship between density, salinity, and temperature has on ocean movement

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5.

Blue food coloring was added so we can see how the water molecules are moving.

Which way does the water move when it is cooled by the ice?

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6.

Which way does the water move when it runs into the end of the tank by the heat lamp?

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17.

What two physical properties of seawater determine whether it rises or sinks?

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18.

Why does melting polar ice risk stopping the global ocean conveyor belt?

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19.

Which of the following global outcomes does the video suggest could happen if ocean currents shut down while global temperatures keep rising?

How would the model change if higher temperatures caused sea ice to melt and the additional fresh water decreased the density of water near the Arctic?

Red arrows represent warm water.

Blue arrows represent cold water.

Large arrows represent fairly quick movement.

Small arrows represent slower movement.

You will use some arrows more than once.