Front — Science definition
Defined in 2 courses:
- A boundary region between air masses with contrasting properties. (Science 6: Matter, Energy & Earth Systems)
- The boundary where two different air masses meet — usually the setting for a region's most active weather. (Earth & Space Science)
Where it is taught
- Atmosphere, Clouds & Weather Records — Water, Air, Weather & Climate, Science 6: Matter, Energy & Earth Systems, Grade 6
- Air Masses, Fronts & Pressure — Atmosphere & Weather, Earth & Space Science, Grade 9
In use
The real drama happens where two air masses meet but refuse to blend, along a boundary called a front.
Air Masses, Fronts & Pressure
Questions using front
Problem 1
- One illustrative result establishes every real condition and needs no further evidence.
- A forecast is a guaranteed observation of the future.
- A noon temperature record automatically gives the whole day’s maximum.
- front: A boundary region between air masses with contrasting properties.
Answer and explanation
front: A boundary region between air masses with contrasting properties.
A boundary region between air masses with contrasting properties. Noon temperature decreases from 19 to 15 °C across the three records. Pressure drops to 1,006 hPa on the rainy day and rises afterward. This small table is consistent with changing weather, but it does not prove pressure alone caused rain, give daily maxima, or establish a rule for every storm.
Problem 2
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 3
Hints
A front does not guarantee identical weather everywhere.
Answer and explanation
Expansion and cooling can bring air to saturation, allowing condensation.
Problem 4
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.