Weather Flashcards
Warm Front
A warm air mass moving over cold air mass, move slower than cold fronts.
Brings less severe weather, but can cause low clouds, ceilings, poor visibility, and rain
Cold Front
A cold air mass moving over a warm air mass, move quicker than warm fronts.
Associated with violent weather, such as sudden storms, gusty winds, turbulence, and occasionally hail or tornadoes
Stationary Front
A cold air mass and warm air mass have met, but neither is taken over by the other
Occluded Front
A cold front catches up to a warm front, where there is warm air above from the warm front and cooler air in front of the warm front
Atmospheric Stability
The airs tendency to either rise and create storms or turbulence(unstable), or to resist vertical movement and motion(stable)
Unstable atmosphere
Air rises easily, more bouyant and turbulent with updrafts and downdrafts, causes the production of clouds, when interacting with a trigger (such as a cold front), more violent weather conditions
Stable Atmosphere
Air resists vertical movement, more prone to fog development at night
Rising Air
When air rises, it expands due to the decrease in pressure, the expansion causes the temp to decrease
Descending Air
Air compresses as it falls, causing an increase in temp
Lapse Rate
The change in temp as altitude increases or decreases
(avg is a 2 degree Celsius drop in temp per 1000ft increase in altitude)
Stable Air Conditions
Cool, dry, and smooth air, poor visibility, and continuous steady precipitation in the presence of larger, low pressure systems.
Favorable conditions in the day in the absence of low pressure systems.
Unstable Air Conditions
Warm, moist air, turbulence, and good visibility, showery precipitation and thunderstorms
Temperature Inversion
Smooth stable air, little to no turbulence.
Occur at low altitudes, not great camera weather, but good flying weather. Continuous steady precipitation
Service Based Temp Inversion
Occurs on a cool clear night when air close to the ground is cooled by the lowering temp of the ground. The air within a few hundred feet of the surface becomes cooler than the air above it
Frontal Temp Inversion
A front of warm air spreads over a layer of cooler air, or a front of cool air is forced under a layer of warm air