4. Air Masses and Fronts Flashcards
Air mass characteristics
Large volume of air, uniform in temp and moisture.
Continental arctic
Dry, very cold, very stable, very low tropopause
Maritime arctic
Moist, cold, unstable in lower levels, low tropopause
Continental polar
Dry, cold, fairly stable, low tropopause
Maritime polar
Moist, warm, unstable, medium tropopause
Continental tropical
Dry, very hot, very unstable, very high tropopause
Maritime tropical
Very moist, hot, very unstable, high tropopause
How are air masses modified?
- Speed that they move
- Moisture/dryness of the region they travel over
- Temp difference between the new surface and the air mass
Warming from below
Develops instability and convection in lower levels
Cooling from below
Causes increased stability in the lower levels
Frontal system definition
Transition zones between air masses where the temp changes rapidly
Naming of frontal systems
Based on the name of the colder air mass involved
Cold front winds (before, while, and after passing)
Southeast-southwest, gusty and shifting, southwest-northwest
Cold front temp (before, while, and after passing)
Warm, sudden drop, steadily dropping
Cold front pressure (before, while, and after passing)
Falling steadily, minimum then sharp rise, rising steadily