A temperature inversion can suppress rising air and limit cloud growth, but sufficiently strong heating or lifting may overcome it.
4 Stability and Storm Development Online Quiz Questions
Use this free practice quiz with 20 questions to review 4 Stability and Storm Development, test your knowledge, and prepare for your next test or exam.
A parcel is lifted in an unstable atmosphere. Which response is most likely?
- A
It is cooler and denser than the surrounding air, so it tends to sink.
- B
It is warmer and less dense than the surrounding air, so it continues rising.
- C
It immediately becomes saturated and stops moving vertically.
- D
It remains at its new level because vertical motion is suppressed.
What is the approximate dry adiabatic cooling rate of a rising unsaturated parcel? Enter the numeric value in °C/km.
What is the name of the level at which a rising air parcel becomes saturated and cloud droplets can begin to form?
After air reaches saturation, water vapor changes into cloud droplets through onto tiny particles in the air.
Which processes can initiate upward motion of air? Select all that apply.
- A
Uneven surface heating that makes air above warmer patches buoyant
- B
Wind pushing air up a mountain or hillside
- C
Denser cold air pushing beneath warmer air at a front
- D
Winds bringing air together near the surface
- E
A temperature inversion forming without any lifting process
A cumulus cloud continues growing upward through a deep layer of unstable air. Which cloud type may it develop into?
- A
Stratus
- B
Small cumulus
- C
Cumulonimbus
- D
Fog
When a saturated parcel rises and water vapor condenses, the process releases , slowing the parcel's cooling.
True or false: In a conditionally unstable atmosphere, an unsaturated parcel may initially be stable but become buoyant after rising enough to become saturated.
- A
True
- B
False
Which ingredients are typically required for thunderstorm development? Select all that apply.
- A
Moisture to supply water for clouds and precipitation
- B
Instability that allows buoyant air to keep rising
- C
A lifting mechanism that starts the ascent
- D
A temperature inversion that cannot be overcome
What happens when cloud particles become too large for the updrafts to keep them aloft?
- A
They remain suspended because cloud particles cannot fall.
- B
They evaporate immediately upon growing.
- C
They fall as rain, snow, or another form of precipitation.
- D
They turn into an updraft.
A storm has a continuing updraft, falling precipitation, and downdrafts developing alongside the updraft. Which stage is it most likely in?
- A
Developing stage
- B
Mature stage
- C
Dissipating stage
- D
Lifting condensation stage
Explain how outflow from a dissipating thunderstorm can weaken that storm yet contribute to new cloud or storm development nearby.
A parcel of air is lifted and then becomes cooler and denser than the air around it. What is the most likely response in a stable atmosphere?
- A
It continues rising because it is warmer and less dense than the surrounding air.
- B
It tends to sink back because it is cooler and denser than the surrounding air.
- C
It remains saturated because lifting prevents its temperature from changing.
- D
It forms a cumulonimbus cloud because all stable air produces strong updrafts.
Wind pushes air up the side of a mountain, where the air expands and cools. Which lifting mechanism is responsible?
- A
Convergence, because winds bring air together near the surface.
- B
Frontal lifting, because dense cold air pushes beneath warmer air.
- C
Orographic lifting, because terrain forces wind-driven air upward.
- D
Surface heating, because the Sun warms the ground unevenly.
Warm, moist air is present near the ground, but a layer warms with height and limits upward motion. What effect can this layer have?
- A
The inversion can act as a cap that limits rising air and delays cloud growth.
- B
The inversion guarantees that surface air will immediately become saturated.
- C
The inversion causes all rising parcels to release latent heat before reaching saturation.
- D
The inversion makes the air above it denser, so precipitation must begin.
A rising parcel reaches saturation and condensation begins. How does this affect the parcel's cooling compared with its unsaturated ascent?
- A
The parcel stops cooling because saturation prevents further expansion.
- B
The parcel cools faster because condensation removes heat from it.
- C
The parcel warms at the dry adiabatic rate because cloud droplets absorb sunlight.
- D
The parcel cools at a lower, variable rate because condensation releases latent heat.
An unsaturated parcel rises, expands, and cools until it becomes saturated and cloud droplets can begin to form. What is the full name of this level?
An unsaturated parcel rises 2 kilometers. Using the approximate dry adiabatic lapse rate of 9.8°C per kilometer, what is its approximate temperature decrease?
True or false: Outflow from a thunderstorm can lift nearby warm, moist air and help new clouds or storms form along the resulting boundary.
- A
True
- B
False
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