
Oceanography part 2
Authored by James Pershin
Science
11th Grade
NGSS covered
Used 1+ times

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19 questions
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1.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Which two factors primarily drive thermohaline circulation?
Wind and tides
Salinity and temperature
Ocean basin shape and Coriolis effect
Atmospheric pressure and density
2.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How does the periodicity of thermohaline circulation affect Earth's climate?
It causes rapid seasonal temperature changes.
It moderates long-term climate cycles over centuries.
It creates sudden increases in polar ice caps.
It leads to faster ocean currents globally.
3.
MULTIPLE SELECT QUESTION
30 sec • 1 pt
Select THREE factors that influence the structure of the oceans and contribute to thermohaline periodicity.
Depth of ocean basins
Salinity variations
Presence of wind currents
Polar ice cap melting
Shape of underwater ridges
4.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
The composition and structure of the oceans lead to thermohaline circulation and its periodicity. Which factors play a role in this process?
Salinity, temperature, and ocean basin structure
Only temperature and salinity
Only ocean basin structure
None of the above
5.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
What happens to thermohaline circulation when polar ice caps melt?
It slows down due to decreased salinity.
It speeds up due to increased salinity.
It reverses direction.
It remains unchanged.
6.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
Click on the two areas of the map showing where melting ice caps most directly impact thermohaline circulation.
Arctic Ocean and North Atlantic Ocean
Indian Ocean and South Pacific Ocean
Mediterranean Sea and Red Sea
Caribbean Sea and Gulf of Mexico
7.
MULTIPLE CHOICE QUESTION
30 sec • 1 pt
How does ocean basin structure influence energy flow in thermohaline circulation?
A. Basin shape funnels currents, affecting their speed.
B. Basin depth reduces salinity differences.
C. Basin structure prevents interaction with surface currents.
D. Basin boundaries create more evaporation.
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