Weather Flashcards
Tropopause
- thin layer above the troposphere
- abrupt change in temperature lapse rate
Stratosphere
- small change in temperature with increasing altitude
The Jet Stream
- “river” of high speed winds (50 knots +)
- winter = south and increased velocity
- summer = north and slower velocity
Standard temperature
15* C at sea level
Average lapse rate
2*C per 1000’
Troposphere
- Surface to 37,000’ (20,000-65,000)
- higher over the equator
- higher in the summer
- Decrease in temperature with increasing alt
Wind rules northern hemisphere
- air circles clockwise around high pressure systems
- air circles counterclockwise around low pressure systems
- closer the isobars together, stronger the wind
- due to surface friction, to about 2000’ winds move outwards from the center of high pressure to low pressure
- coriolis effect deflects wind to the right
Relative humidity
- how much water vapor thats present in the air vs. how much it can actually hold
- 100% is considered “saturated
- warm air can hold more water vapor than cold air
Dew point
The temperature air must cool too to become saturated (100%) by the water already present in the air
Wet snow
- temperature is above freezing at your altitude
Atmospheric stability
The resistance of the atmosphere to vertical motion.
Characteristics of unstable air
Cumuliform clouds, showery precipitation, rough air (turbulence), and good visibility
Characteristics of stable air
Stratiform clouds and fog, continuous precipitation, smooth air, and fair to poor visibility in haze and smoke
Dry adiabatic lapse rate
3*C per 1,000’
Family’s of clouds
- high clouds
- middle clouds
- low clouds
- clouds with extensive vertical development