Fronts Part 2(oxford) Flashcards
Air masses are identified by temperature/latitude, these include:
and by humidity or sea/land source:
- Equatorial.
- Tropical.
- Polar.
- Arctic.
- Equatorial.
- Tropical.
- Polar.
- Arctic.
Air masses:
Arctic Maritime :
- Source
- Stability
- Temperature
- Moisture
- Time of the year
- Weather
- Polar ice cap
- Stable
- Very cold
- Dry
- September and May
- Humidity increase as it moves over the Norwegian sea, becoming very unstable. Large CU and CB.
Air masses:
Polar Maritime:
- Source
- Stability
- Temperature
- Moisture
- Time of the year
- Weather
- Northwest, North Atlantic
- Stable
- Cold
- Absolute humidity low, relative humidity high
- -
- Approaching inland becomes unstable with CU and CB
Air masses:
Polar Continental :
- Source
- Stability
- Temperature
- Moisture
- Time of the year
- Weather
- Siberia
- Stable
- Cold
- Dry
- -
- If from the east travelling over continental Europe, then very cold, very dry, no
cloud, no precipitation. If the airflow comes over the Baltic or North Seas the air will become unstable, with large
Cu and heavy snow showers on the E coast of Sweden and the UK. Remains very cold. In summer the air mass virtually disappears. However, with high pressure over Scandinavia in early to mid summer, there will be a NE flow over the North Sea to E UK. The air originates as dry, warm and stable. Over the North Sea it becomes moist and cool. This results in Haar conditions over E coast of N England and Scotland - very low St, drizzle, advection fog, poor visibility.
Air masses:
Tropical Continental:
- Source
- Stability
- Temperature
- Moisture
- Time of the year
- Weather
- N Africa/SE Europe.
- Stable
- Warm
- Dry
- Summer
- No cloud or precipitation, warm or very warm. Visibility
moderate except in dust haze which can occur.
Air masses:
Tropical Maritime:
- Source
- Stability
- Temperature
- Moisture
- Time of the year
- Weather
- The Azores anticyclone
- Stable
- warm
- RH high, AH high.
- -
- Low cloud, St and Sc. Drizzle or light precipitation. Visibility poor. Advection fog over sea area late spring, early summer, over land winter, early spring. In high summer insolation and convection break down the stability resulting in clear skies or possibly a few small Cu
The main global fronts are:
Fronts in a locality are named
- The Polar Front.
- The Arctic Front.
- The Mediterranean Front.
- The Intertropical Convergence Zone (ITCZ).
• Cold or warm
Frontal surfaces which are in equilibrium with no tendency for
the cold air to undercut the warm, thus not convergence, is called -
quasi-stationary front
If warm air is replacing cold air, then the front is called -
Warm front
A warm front has an approximate slope of -
The slope of a cold front is approximately -
1: 150
1: 50 to 1:80
If cold air is replacing warm air, then the front is called a -
cold front
Clouds associated with a warm front -
CI, CS, AS, NS and SC.
Clouds associated with a cold front -
CU, CB and AC
The area lying between the two fronts is known as -
The type of weather -
The warm sector
Stratus and stratocumulus
Ahead of a warm front:
Surface W/V - Temperature - Dew Point - Pressure - Cloud - Precipitation - Visibility -
Surface W/V - Speed increasing, slight backing, usually southerly.
Temperature - Steady low.
Dew Point - Steady low.
Pressure - Steady fall.
Cloud - Increasing to 8/8, base lowering, Ci, Cs, As, Ns.
Precipitation - Light continuous from As becoming moderate to heavy continuous from Ns.
Visibility - Reducing to poor.