Air Masses and Source Regions Flashcards
Fronts
boundaries between different air masses
Air Mass
large volumes of air with uniform temperature and humidity
Source Regions
areas of the globe where air masses form
-air must remain over a source region for substantial length of time for an air mass to form
Basic Characteristics
- Moisture
a. continental; forming over land, dry
b. maritime; forming over ocean, humid - Temperature
a. tropical; forming near the tropics in lower altitudes, warm
b. Polar; cold
c. Arctic; very cold
Maritime Polar from Gulf of Alaska
-originates from Gulf of Alaska and grates down along the west coast of North America
-cold, humid, unstable
-trajectory into US depends on the position of the polar jet stream
a. when jet stream is dipping southward LA has poor weather, when facing northward LA has clear weather
-maritime polar air coming from the ocean gets enhanced as they are lifted up the mountain range and leads to precipitation
-large source of winter precipitation in California
How does the jet stream change in the winter
it moves to the south and become stronger and the waves become more pronounced
Maritime Polar from Atlantic
-cold, humid, unstable
-nor’easters
Nor’easters
-dumps a lot of snow in New England
-caused when the polar het stream transports cold arctic air from Canada and meets with warm air from the Gulf of Mexico … when these meet over the cold Atlantic it leads to nor’easters
Maritime Tropical
-warm, humid
-major source of precipitation and thunderstorms in the southeastern US
Atmospheric Rivers
-relatively long. narrow regions in the atmosphere that transport most of the water vapor outside of the tropics
-air masses forming in maritime tropical region in the pacific that bring in warm humid maritime tropical air and carry high amounts of water vapor
-second major source of precipitation in California
-Pineapple Express from Hawaii
Atmospheric River Synoptic Pattern Development
- 7-10 days before event there is a ridge that is locked over west coast that prevents precipitation in SoCal, but heavy rain over western pacific
- 2-5 days before event the ridge starts to break down because the jet split and from two jets; this opens up a southern corridor that allows the jet to route in weather off the pacific
- Precipitation Event: southern portion of the jet stream takes over and allows the routing of the atmospheric river towards SoCal
Why can’t air masses form in mid-latitudes?
They are too variable and don’t have quiet periods
What happens when an air mass moves?
- The region in which the air moves undergoes a major change in temperature and humidity
- The air mass becomes more moderate
How do cP air masses differ in the winter vs the summer?
In the winter snow radiation leads to cool temp that create stable conditions — prevents cloud formation so usually bright and sunny
More humid in the summer and leads to cumulus clouds but not much precipitation
Where do cT air masses usually form?
in deserts over the Southwestern US and Northern Mexico
*unstable because of dryness