Ocean Circulation & Climate — Drills · Grade 9 Science
Chapter: Oceans, Carbon & ClimateWhat these drills covers
By the end of Ocean Circulation & Climate you should be able to:
- I can distinguish wind-driven surface circulation from density-driven movement.
- I can explain how ocean energy storage and transport affect climate.
8 questions, multiple choice and written answer, each with a worked explanation.
Vocabulary used: salinity, stratification, heat capacity.
Problem 1
- less dense
- more dense
- massless
- always freeze instantly
Answer and explanation
more dense
Dissolved salts generally increase seawater density.
Problem 2
Answer and explanation
It hides variable pathways, mixing, regional differences, and changes over time.
Problem 3
- tides
- prevailing winds
- earthquakes
- the Moon's phases
Answer and explanation
prevailing winds
Wind dragging on the surface sets the large gyres in motion.
Problem 4
- colour
- temperature and salinity, and therefore density
- wave height
- depth alone
Answer and explanation
temperature and salinity, and therefore density
Cold, salty water is denser and sinks, driving the deep overturning.
Problem 5
- colder
- milder
- drier always
- unchanged
Answer and explanation
milder
The current carries heat that moderates coastal temperatures.
Problem 6
- warms and freshens
- cools and becomes saltier
- warms and becomes saltier
- is stirred
Answer and explanation
cools and becomes saltier
Both lower temperature and higher salinity increase density.
Problem 7
Answer and explanation
When seawater freezes, most of the salt is excluded from the ice and left in the water below, raising its salinity. That water is also very cold, so it becomes dense enough to sink. The sinking drives the deep limb of the overturning circulation, which is why polar regions are where the deep ocean is renewed.
Response criteria
- State a scientifically accurate conclusion.
- Show the data, mechanism, or calculation that supports it.
- Include units, conditions, or limits where relevant.
Problem 8
Answer and explanation
The ocean stores far more heat than the atmosphere and moves it over long distances, so currents redistribute energy from the tropics toward the poles and moderate the climates of coasts they pass. Changes in that circulation therefore change regional climate, which is why it is monitored as closely as the atmosphere.
Response criteria
- State a scientifically accurate conclusion.
- Show the data, mechanism, or calculation that supports it.
- Include units, conditions, or limits where relevant.