Multiple Choice 1
Multiple choice 2
Vocab 1
Vocab 2
100

Which process most directly causes ocean acidification?
 
A. Increased ocean temperatures
 
B. Absorption of atmospheric carbon dioxide
 
C. Overfishing of shellfish
 
D. Large-scale plastic pollution

 B. Absorption of atmospheric carbon dioxide
 

100

Thermohaline circulation helps regulate climate by:
 
A. Preventing any ocean movement
 
B. Transporting heat between equator and poles
 
C. Stopping storms from forming
 
D. Increasing the number of fish everywhere

B. Transporting heat between equator and poles

100

When deep, cold, nutrient-rich water rises to the surface.

Carbon Sink 

 Salinity 

Heat Capacity  

Sea Surface Temperature 

Upwelling

 

 

Upwelling

100

A steady flow of ocean water moving in a specific direction.

Density  

Current

Thermohaline Circulation  

Evaporation 

Precipitation 

Current

200

Thermohaline circulation is primarily driven by differences in:
 
A. Wind speed and direction
 
B. Water density caused by temperature and salinity
 
C. Tidal forces from the moon
 
D. Surface current eddies

B. Water density caused by temperature and salinity

200

Which factor most directly limits primary productivity in much of the open ocean?
A. High water temperature
 
B. Low nutrient availability
 
C. Excess light
 
D. High biodiversity

B. Low nutrient availability

200

A place that absorbs and stores carbon dioxide, like the ocean. 

Carbon Sink 

Salinity 

Heat Capacity  

Sea Surface Temperature 

Upwelling

Carbon Sink 

200

How tightly packed matter is in a substance. In the ocean, denser water sinks below less dense water.

Density  

Current 

Thermohaline Circulation  

Evaporation 

Precipitation

Density  

300

Which process returns nutrients to the water column after organisms die?
A. Photosynthesis
 
B. Evaporation
 
C. Decomposition
 
D. Respiration by phytoplankton

C. Decomposition

300

Which human activity most directly reduces coastal habitats like mangroves and salt marshes?
 
A. Coastal development and land reclamation
 
B. Offshore wind farms
 
C. Deep-sea mining
 
D. Recreational boating

A. Coastal development and land reclamation

300

The ability of a substance to store heat 

Carbon Sink 

Salinity 

Heat Capacity  

Sea Surface Temperature 

Upwelling

Heat Capacity  

300

The process of liquid water turning into water vapor (gas)

Density  

Current 

Thermohaline Circulation  

Evaporation

Precipitation

Evaporation

400

Why does forming sea ice increase the salinity of the surrounding seawater?
 
A. Salt is expelled from freezing water and stays in the liquid  
 
B. Ice adds salt to the water
 
C. Ice lowers water temperature but not salinity
 
D. Sea ice attracts freshwater from rivers

A. Salt is expelled from freezing water and stays in the liquid  

400

Evaporation from the ocean primarily contributes to which atmospheric process? 

A. Decreasing air pressure 

B. Reducing wind speed  

C. Reflecting sunlight back to space 

D. Increasing atmospheric moisture and cloud formation

D. Increasing atmospheric moisture and cloud formation

400

The amount of salt dissolved in water.

Carbon Sink 

Salinity

Heat Capacity  

Sea Surface Temperature 

Upwelling

Salinity

400

Water that falls from the atmosphere to Earth, such as rain or snow.

Density  

Current 

Thermohaline Circulation  

Evaporation 

Precipitation

Precipitation

500

Which process brings cold, nutrient-rich deep water to the surface?
 
A. Downwelling
 
B. Upwelling
 
C. Evaporation
 
D. Condensation

B. Upwelling

500

Why do coastal areas often have smaller temperature ranges between day and night compared to inland areas? 

A. Coastal areas receive more solar radiation 

B. The ocean absorbs and releases heat slowly, moderating temperature changes

C. Coastal areas have stronger winds that cool the land 

D. The ocean increases the land’s ability to reflect heat 

B. The ocean absorbs and releases heat slowly, moderating temperature changes

500

The temperature of the ocean’s top layer of water. 

Carbon Sink 

Salinity 

Heat Capacity  

Sea Surface Temperature

Upwelling

Sea Surface Temperature

500

The global movement of deep ocean water driven by differences in temperature (thermo) and salinity (haline)

Density  

Current 

Thermohaline Circulation  

Evaporation 

Precipitation

Thermohaline Circulation  

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