Match the term with its description regarding air mass stability.
| A. Air that resiste vertical motion, leading to layered clouds and smooth air |
| B. Air that promotes vertical motion, leading to thunderstorms and turbulent air |
| C. Air that is stable for unsaturated air, but becomes unstable when saturated |
A1 - a, 2-b, 3 -c
B1 - b, 2-a, 3-c
C1-c, 2-a, 3-b
D1-a, 2-c, 3-b
Answer:
A. 1 - a, 2-b, 3 -c
Read Explanation:
Understanding Air Mass Stability
Stable Air Mass
A stable air mass is characterized by its resistance to vertical motion. When a parcel of air is lifted in a stable environment, it becomes cooler and denser than the surrounding air, causing it to sink back to its original position.
Key Indicators:
Leads to the formation of stratiform clouds (e.g., stratus, nimbostratus) which are flat, layered, and often cover large areas.
Precipitation from stable air masses is typically light, continuous, and widespread (e.g., drizzle or light rain).
Visibility tends to be poor due to the trapping of smoke, haze, and fog near the surface.
Aircraft experience smooth, non-turbulent conditions.
Atmospheric Condition:
Occurs when the Environmental Lapse Rate (ELR) is less than the Moist Adiabatic Lapse Rate (MALR), meaning the air temperature decreases slowly with height. This is known as absolute stability.
Unstable Air Mass
An unstable air mass promotes vigorous vertical motion. When a parcel of air is lifted in an unstable environment, it remains warmer and less dense than the surrounding air, causing it to continue rising.
Key Indicators:
Results in the formation of cumuliform clouds (e.g., cumulus, cumulonimbus) which are vertically developed, often towering clouds.
Precipitation is typically showery, intense, and localized, often associated with thunderstorms, hail, or even tornadoes.
Visibility is generally good (outside of precipitation) due to strong vertical mixing dispersing pollutants.
Aircraft experience turbulent conditions.
Atmospheric Condition:
Occurs when the Environmental Lapse Rate (ELR) is greater than the Dry Adiabatic Lapse Rate (DALR), meaning the air temperature decreases rapidly with height. This is known as absolute instability.
Conditional Air Stability (Conditional Instability)
Conditional stability describes a situation where the atmosphere is stable if the air is unsaturated (dry) but becomes unstable if the air becomes saturated (wet).
Key Concept:
This state exists when the Environmental Lapse Rate (ELR) is greater than the Moist Adiabatic Lapse Rate (MALR) but less than the Dry Adiabatic Lapse Rate (DALR).
If an unsaturated air parcel is lifted, it cools at the DALR, which is faster than the ELR, making it stable.
However, if the air parcel becomes saturated (e.g., reaches its lifting condensation level), it cools at the slower MALR. If the MALR is less than the ELR, the saturated parcel will continue to rise, leading to instability.
Weather Implications:
This is a very common atmospheric condition that allows for the development of thunderstorms when sufficient moisture and a lifting mechanism (like a front or orographic lift) are present to saturate the air.
