Storms Review
Air Parcel
- for an air parcel to rise, it must be warmer (and therefore, less dense) than the air around it
- once it starts to rise, it cools
- increases air parcels relative humidity
- absolute humidity stays the because that is just the total amount of water vapor in the air
- when an air parcel reaches a relative humidity of 100%, it’s saturated with water
- this is called the dew point
- once the air parcel cools lower than the dew point, the water will condense and precipitation will occur
- this condensation causes energy to be released as latent heat
- as an air parcel rises through the atmosphere, the relative humidity will increase
Storms
when two air masses (one cold and one warm) collide, a severe thunderstorm is produced
air-mass:
- key criteria required to form it:
- inflow of warm, moist air (like tropical climates or late afternoons in the summer)
- characteristics that differentiate it from other thunderstorm types:
- local thunderstorms and only last for a short amount of time
severe:
key criteria required to form it:
two air masses (a cold and warm front) collide to cause more intense updrafts of warm air and resulting downdrafts of cold air
characteristics that differentiate it from other thunderstorm types:
must have either:
- high winds (>58 mph)
- large hail (at least 1” diameter)
- generate a tornado/tornadoes
supercell:
- key criteria required to form it:
- extremely large updrafts of warm air
- rotation of the updrafts to create a vortex
- characteristics that differentiate it from other thunderstorm types:
- rotation of the updrafts and tilting of the storm are key criteria that differentiate it from a severe thunderstorm