Stability of the atmosphere

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University
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1.
FLASHCARD QUESTION
Front
What is atmospheric stability?
Back
Atmospheric stability refers to the tendency of air parcels to either rise or sink in the atmosphere. It is determined by the temperature difference between the air parcel and the surrounding environment.
2.
FLASHCARD QUESTION
Front
What are the three types of atmospheric stability?
Back
1. Positive Stability: Air parcels are cooler than their environment and sink. 2. Negative Stability: Air parcels are warmer than their environment and rise. 3. Neutral Stability: Air parcels have the same temperature as their environment and neither rise nor sink.
3.
FLASHCARD QUESTION
Front
What happens to a rising parcel of air when it reaches its saturation point?
Back
When a rising parcel of air reaches its saturation point, it can no longer hold all the moisture, leading to condensation and potentially precipitation.
4.
FLASHCARD QUESTION
Front
What is the significance of the ambient temperature in atmospheric stability?
Back
The ambient temperature determines whether a rising or sinking air parcel will continue to rise or sink. If the parcel's temperature exceeds the ambient temperature, it will continue to rise.
5.
FLASHCARD QUESTION
Front
What is the Dry Adiabatic Lapse Rate?
Back
The Dry Adiabatic Lapse Rate is the rate at which unsaturated air cools as it rises, approximately 10°C per kilometer.
6.
FLASHCARD QUESTION
Front
What is the Saturated Adiabatic Lapse Rate?
Back
The Saturated Adiabatic Lapse Rate is the rate at which saturated air cools as it rises, typically around 6°C per kilometer.
7.
FLASHCARD QUESTION
Front
How does relative humidity affect atmospheric stability?
Back
High relative humidity can lead to instability as it increases the likelihood of condensation and cloud formation, which can enhance rising air parcels.
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