If an atmosphere is stable to convection, it means a rising air parcel will be (choose all correct answers):

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BlackTom AI · Accepted Answer

When assessing stability to convection, we ask what happens to a parcel that starts to rise. If the atmosphere is stable, a parcel that is lifted will tend to return to its original level rather than continue rising.
Option 1: less dense than the surrounding air — this would make the parcel buoyant and cause it to keep rising, which contradicts stability. A stable atmosphere does not support a rising, less-dense parcel.
Option 2: warmer than the surrounding air — a warmer parcel is lighter and would rise on its own, again implying instability. This is not consistent with a stable stratification.
Option 3: colder than the surrounding air — a cooler parcel is denser than its environment, so it will slow its ascent and tend to sink back or stop rising, aligning with stability.
Option 4: denser than the surrounding air — increased density relative to the environment makes the parcel negatively buoyant, reinforcing the tendency to resist or stop rising, which matches stable conditions.
In summary, for an atmosphere stable to convection, rising parcels are typically denser and colder than their surroundings, causing them to stall or sink back rather than continue rising.

CLMTGR5001_002_2025_3 - Dynamics of Climate Variability and Chan Midterm Group A (Secure Browser)

If an atmosphere is stable to convection, it means a rising air parcel will be (choose all correct answers):

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CLMTGR5001_002_2025_3 - Dynamics of Climate Variability and Chan Midterm Group A (Secure Browser)

If an atmosphere is stable to convection, it means a rising air parcel will be (choose all correct answers):

View Explanation

Log in for full answers

Similar Questions

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A conditionally unstable atmosphere is with respect to unsaturated air and with respect to saturated air.