Air Masses, Fronts & Pressure — Practice · Grade 9 Science
Chapter: Atmosphere & WeatherWhat this practice covers
By the end of Air Masses, Fronts & Pressure you should be able to:
- I can classify an air mass by where it formed, using the terms continental, maritime, polar, and tropical.
- I can compare how cold fronts and warm fronts differ in speed and the weather they bring.
- I can relate high and low air pressure to sinking/rising air and fair/stormy weather.
11 questions, multiple choice and written answer, each with a worked explanation.
Vocabulary used: air mass, front, air pressure, barometer.
Problem 1
- Cold and dry
- Cold and moist
- Warm and dry
- Warm and moist
Answer and explanation
Cold and dry
'Continental' means it formed over land (dry), and 'polar' means it formed at a cold latitude.
Problem 2
- Front
- Barometer
- Isobar
- Station model
Answer and explanation
Front
The boundary between two air masses is a front — it's where the most active weather usually happens.
Problem 3
- Cold fronts move fast and bring brief, intense weather; warm fronts move slowly and bring longer, lighter weather.
- Cold fronts move slowly and bring long light rain; warm fronts move fast and bring brief storms.
- Both move at the same speed and bring identical weather.
- Warm fronts only occur in summer.
Answer and explanation
Cold fronts move fast and bring brief, intense weather; warm fronts move slowly and bring longer, lighter weather.
Cold fronts are steep and fast-moving, causing quick, intense weather; warm fronts are gradual and slow-moving, causing longer, gentler weather.
Problem 4
- High pressure
- Low pressure
- A stationary front
- An occluded front
Answer and explanation
High pressure
Sinking air piles up near the ground, creating high pressure and generally fair weather.
Problem 5
- A low-pressure system, with cloudier, stormier weather ahead
- A high-pressure system, with clear, calm weather ahead
- No change in the weather at all
- A broken barometer
Answer and explanation
A low-pressure system, with cloudier, stormier weather ahead
A reading well below the roughly 1013-millibar average indicates lower-than-average pressure, which is associated with rising air and increasing clouds or storms.
Problem 6
Answer and explanation
Air naturally flows from where it is denser and pressing down harder (high pressure) toward where it is less dense and pressing down less (low pressure), trying to balance out the difference — that flow of air from high to low is what we feel as wind.
Problem 7
Answer and explanation
A passing cold front is plausible; a map and additional observations would test it.
A cooler air mass replacing warmer air fits the temperature drop.
The wind shift and precipitation add supporting evidence.
Response criteria
- Use the stated conditions.
- Show the evidence or calculation.
- Explain the conclusion and any stated limitation.
Problem 8
Hints
A front does not guarantee identical weather everywhere.
Answer and explanation
Expansion and cooling can bring air to saturation, allowing condensation.
Problem 9
Hints
State what the supplied observations or conditions establish, and separate that from any assumption.
Answer and explanation
Temperature, humidity, origin region and movement provide important context.
Problem 10
Answer and explanation
Available moisture, stability, local flow and timing vary. Lifting supplies a process, while those conditions influence whether and how precipitation develops.
Trace the cool-air advance separately from the warmer-air uplift. The sloping boundary is a schematic cold front, not an identical geometry for every front.
Available moisture, stability, local flow and timing vary. Lifting supplies a process, while those conditions influence whether and how precipitation develops.
Response criteria
- Read the labeled quantities, reference frame or objects correctly.
- Explain the relation between the visual evidence and the mechanism.
- Keep the drawing’s stated assumptions and limits in the conclusion.
Problem 11
Answer and explanation
A is 0.04 hPa/km; B is 0.08 hPa/km, twice as large. Actual wind also responds to rotation and friction, so pressure-gradient magnitude alone is not a complete directional forecast.
Calculate 4/100 and 2/25 in matched units.
Compare 0.08 with 0.04: factor two.
Include rotation/friction and distinguish pressure-gradient force from wind.
Response criteria
- Use the stated measurements or conditions, with correct units.
- Connect the result to the physical mechanism or evidence relationship.
- Identify the assumption, model limit or further evidence requested.