Atmospheric Energy & Circulation — Drills · Grade 9 Science
Chapter: Atmosphere & WeatherWhat these drills covers
By the end of Atmospheric Energy & Circulation you should be able to:
- I can explain how unequal solar heating drives atmospheric circulation.
- I can trace energy through radiation, convection, and phase changes.
8 questions, numeric, written answer and multiple choice, each with a worked explanation.
Vocabulary used: albedo, convection, latent energy transfer.
Problem 1
Answer and explanation
30 %
30 ÷ 100 × 100 = 30.
Problem 2
Answer and explanation
It deflects motion relative to the surface and helps organize circulation patterns.
Problem 3
- heavier
- less dense than the cooler air around it
- attracted upward
- pushed by the Sun
Answer and explanation
less dense than the cooler air around it
Heating expands air, lowering its density so it is buoyant.
Problem 4
- from further away
- more directly
- through more atmosphere
- at night
Answer and explanation
more directly
A steeper angle concentrates the same beam on a smaller area.
Problem 5
- uneven heating between equator and poles
- the Moon
- ocean salinity
- volcanoes
Answer and explanation
uneven heating between equator and poles
The temperature difference drives air to move, redistributing energy.
Problem 6
- convection
- the Coriolis effect
- conduction
- radiation
Answer and explanation
the Coriolis effect
It is why winds curve rather than flowing straight from high to low pressure.
Problem 7
Answer and explanation
Air that rose at the equator and lost its moisture as rain travels poleward aloft and descends around 30°. Descending air warms and its relative humidity falls, so cloud and rain are suppressed. The dryness is a consequence of the circulation pattern rather than of local conditions, which is why deserts appear at similar latitudes on several continents.
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
Air heated at the equator rises and flows poleward at altitude, carrying energy with it as both temperature and latent heat in water vapour. It cools, descends and returns toward the equator near the surface. Storm systems in the mid-latitudes carry further energy poleward. Without this transport the tropics would be far hotter and the poles far colder than they are.
Response criteria
- State a scientifically accurate conclusion.
- Show the data, mechanism, or calculation that supports it.
- Include units, conditions, or limits where relevant.