Impact of Wind on Ocean Dynamics

Impact of Wind on Ocean Dynamics

Assessment

Interactive Video

Science, Geography, Biology

9th - 10th Grade

Hard

Created by

Patricia Brown

FREE Resource

The video explains ocean temperature fluctuations caused by upwelling and downwelling, driven by wind patterns and the Coriolis effect. It covers Ekman transport, mesoscale eddies, and their impact on ocean circulation. The video also discusses the economic significance of these phenomena, particularly in fisheries, and their influence on global climate patterns.

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10 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What causes the fluctuations in ocean temperatures at the Jersey Shore?

Seasonal changes

Global warming

Upwelling and downwelling

Tidal waves

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

In the northern hemisphere, how does the Coriolis effect influence water movement?

Water spirals upwards

Water moves in a straight line

Water deflects 90 degrees to the right

Water deflects 90 degrees to the left

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What happens to water when winds push it away from the coast?

Water remains stagnant

Coastal upwelling occurs

Water temperature increases

Coastal downwelling occurs

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What is Ekman transport?

Horizontal movement of water due to wind stress

Vertical movement of water

Temperature-induced water movement

Circular movement of water

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

What are mesoscale eddies?

Small ocean circulations influenced by temperature gradients

Deep ocean trenches

Small atmospheric circulations

Large ocean currents

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

How does the curvature of the coast affect upwelling and downwelling?

It reverses the effect

It maximizes the effect

It minimizes the effect

It has no effect

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

During an El Niño event, what occurs along the eastern Pacific coast of South America?

Upwelling

Increased salinity

Downwelling

No change

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