Air Masses and Source Regions Flashcards

1
Q

Fronts

A

boundaries between different air masses

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1
Q

Air Mass

A

large volumes of air with uniform temperature and humidity

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2
Q

Source Regions

A

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

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3
Q

Basic Characteristics

A
  1. Moisture
    a. continental; forming over land, dry
    b. maritime; forming over ocean, humid
  2. Temperature
    a. tropical; forming near the tropics in lower altitudes, warm
    b. Polar; cold
    c. Arctic; very cold
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4
Q

Maritime Polar from Gulf of Alaska

A

-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

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5
Q

How does the jet stream change in the winter

A

it moves to the south and become stronger and the waves become more pronounced

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6
Q

Maritime Polar from Atlantic

A

-cold, humid, unstable
-nor’easters

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7
Q

Nor’easters

A

-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

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8
Q

Maritime Tropical

A

-warm, humid
-major source of precipitation and thunderstorms in the southeastern US

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9
Q

Atmospheric Rivers

A

-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

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10
Q

Atmospheric River Synoptic Pattern Development

A
  1. 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. 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
  3. Precipitation Event: southern portion of the jet stream takes over and allows the routing of the atmospheric river towards SoCal
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11
Q

Why can’t air masses form in mid-latitudes?

A

They are too variable and don’t have quiet periods

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12
Q

What happens when an air mass moves?

A
  1. The region in which the air moves undergoes a major change in temperature and humidity
  2. The air mass becomes more moderate
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13
Q

How do cP air masses differ in the winter vs the summer?

A

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

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14
Q

Where do cT air masses usually form?

A

in deserts over the Southwestern US and Northern Mexico

*unstable because of dryness

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