Test 3 Flashcards
What are source regions?
- Latitude P = Polar T = Tropical
- Underlying Surface m = maritime c = continental
Geostrophic wind
An upper level wind that flows parallel to the isobars
When we reach geostrophic conditions
The Coriolis force is equal to the pressure gradient force
Two main jet streams
PFJ (polar front jet) and STJ (sub tropical jet)
PFJ
Is variable in character, Strength varies daily, weekly, seasonally, Position varies daily, Controls surface weather, Controls movement of surface pressure cells
STJ
Is not seasonal in nature, Geographically stable
Meteorologically less important, but, climatologically important (linked to position of STH)
Jet streams length
Thousands of miles long, hundreds of miles wide, only a few miles thick
Jet streams location
Located between 9000m and 15000m (roughly 30-50 thousand feet)
Jet stream speed
Average wind velocity 75mph, can exceed 250mph (60 knots is threshold for classification)
Jet streams form
In zones of maximum thermal and pressure gradients at top of troposphere
Polar Front Jet Stream
Strongest in winter, weakest in summer,
Shifts equator ward in winter, poleward in summer
Air masses form
Over thermal characteristics from source regions
4 main air masses
cP – continental Polar
mP – maritime Polar
mT – maritime Tropical
cT – continental Tropical
Air masses size
Size: subcontinental (~1000 km diameter)
Size vertical: from surface through troposphere