True or false: The Coriolis effect starts the wind by pushing air from one place to another.
3 Pressure and Atmospheric Circulation Online Quiz Questions
Use this free practice quiz with 20 questions to review 3 Pressure and Atmospheric Circulation, test your knowledge, and prepare for your next test or exam.
On a weather map, one region has closely spaced isobars and another has widely spaced isobars. All else being equal, where would you expect the stronger pressure-gradient force and faster winds?
- A
The widely spaced isobars indicate the steeper pressure gradient, so winds should be faster there.
- B
The closely spaced isobars indicate the steeper pressure gradient, so winds should be faster there.
- C
The spacing of isobars indicates pressure but gives no information about the pressure gradient.
Air moves north in the Northern Hemisphere. In which compass direction is it deflected by the Coriolis effect?
During the day, land beside a coast warms faster than the water. What is the name of the surface breeze that flows from the water inland?
Which description best matches the average surface flow in the Ferrel cell?
- A
Surface air flows equatorward and is deflected westward, forming polar easterlies.
- B
Surface air flows poleward and is deflected eastward, forming the prevailing westerlies.
- C
Surface air flows toward the equator and is deflected eastward, forming the trade winds.
True or false: In the simplified three-cell model, the circulation cells form fixed boundaries that do not shift with season.
- A
True
- B
False
Near the ground, how does wind typically flow around a low-pressure center when friction weakens the Coriolis effect?
- A
It flows directly outward across isobars because the Coriolis effect is strongest near the ground.
- B
It flows parallel to isobars and circles the low without crossing them.
- C
It crosses isobars toward lower pressure and spirals inward around the low.
Select all statements that accurately describe the simplified three-cell circulation model.
- A
In the Hadley cell, air rises near the equator and generally sinks in the subtropics.
- B
In the Ferrel cell, average surface flow is poleward and forms prevailing westerlies after deflection.
- C
In the Polar cell, cold air tends to sink over the poles and flow toward lower latitudes near the surface.
- D
The Ferrel cell is a direct loop driven only by air rising at the equator and sinking at the poles.
Select all factors identified as modifying the broad patterns of global atmospheric circulation.
- A
Seasonal shifts in solar heating.
- B
Earth's rotation.
- C
The distribution of land and ocean.
- D
Fixed latitude lines that keep every circulation pattern unchanged throughout the year.
Compare typical near-surface wind flow around low- and high-pressure centers. Then explain how the usual vertical air motion near each center can affect cloud formation, without treating the outcomes as certain.
A weather station is moved to a higher elevation. Based on the general relationship between altitude and atmospheric pressure, what change would you expect?
- A
Pressure tends to be higher because more air lies above the station.
- B
Pressure tends to be lower because less air lies above the station.
- C
Pressure must remain the same because elevation does not affect atmospheric pressure.
A weather map shows isobars much closer together in one region than in a nearby region. All else being equal, what does this suggest about winds in the region with closer isobars?
- A
The pressure gradient is weaker, so winds should be slower.
- B
The pressure gradient is stronger, so winds should be faster.
- C
The pressure gradient is unchanged, but wind direction must reverse.
- D
The air pressure is equal everywhere between the isobars.
A pressure difference helps drive wind, while the Coriolis effect changes the direction of air that is already moving.
- A
True
- B
False
At night, a coastal area experiences near-surface air flowing from the cooler land toward the water. What is this wind called?
Air is moving northward in the Northern Hemisphere. In which direction does the Coriolis effect deflect it relative to its path?
- A
Westward, so it turns left of its path.
- B
Southward, so it moves back toward the equator.
- C
Eastward, so it turns right of its path.
- D
It is not deflected because it is moving north.
On a sunny afternoon, land beside a coast heats faster than the nearby water. Which near-surface circulation is most likely to develop?
- A
A sea breeze, with near-surface air moving from water toward land.
- B
A land breeze, with near-surface air moving from land toward water.
- C
A mountain breeze, with air draining downslope.
- D
A valley breeze, with air moving down-valley.
During the day, air warmed along mountain slopes flows upslope and up-valley. What is this wind called?
In the simplified three-cell model, which circulation zone is associated with average midlatitude surface flow that moves poleward and is deflected eastward?
- A
Hadley cell: its surface flow returns toward the equator.
- B
Ferrel cell: its average surface flow is poleward and deflected eastward.
- C
Polar cell: its surface flow is deflected eastward to form trade winds.
- D
Hadley cell: its surface flow moves from the poles toward 60° latitude.
At night, cooled, denser air drains and ; this circulation is called a mountain breeze.
In the simplified three-cell model, cold air sinks over the poles and flows toward lower latitudes near the surface. Air generally rises again near latitude.
Related study packs and tools
- Study guide
1 Patterns and Causes of Population Distribution
Learn how population is distributed across the world and within regions, how density and settlement patterns are described, and how physical and human influences shape where communities grow or decline.
- Study guide
13. Human–Environment Interaction and Geographic Synthesis
A structured guide to how physical environments and human decisions interact across population, migration, culture, politics, agriculture, cities, and geographic analysis.
AP Human GeographyUpdated - Study Pack
AP Human Geography
Students study systematic patterns of human population dynamics, migration trends, cultural landscapes, political organization, and agricultural/urban land use. The course highlights how humans shape and are affected by their physical environments.
39 study toolsUpdated - Study Pack
Human Geography: Population Geography
Focused study of population distribution, density and demographic transitions.
9 study toolsUpdated - Study Pack
Physical Geography: Climate
Focused study of climate controls, climate zones and long-term patterns.
12 study toolsUpdated - Study Pack
Physical Geography: Ecosystems
Focused study of energy flows, ecological interactions and biome distributions.
12 study toolsUpdated - Study Pack
Physical Geography: Landforms and Geomorphology
Focused study of weathering, erosion, deposition and landform development.
12 study toolsUpdated - Study Pack
Physical Geography: Soils
Focused study of soil formation, horizons, properties and erosion.
12 study toolsUpdated - Study Pack
Physical Geography: Water Systems
Focused study of the hydrologic cycle, rivers, groundwater and drainage.
18 study toolsUpdated