Atmosphere Disturbance Pt 1 Flashcards

1
Q

Air mass

A

parcel of air:
1) large
2) uniform in horizontal dimension
3) travels as unit

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2
Q

effect of Latitude on air mass

A

IF air mass forms OVER:
low-latitude air mass = warm/hot + unstable
high latitude = cool/cold more stable
over ocean = moist
over continental surface = dry

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3
Q

A Air mass

A

Arctic/Antarctic = A = formed over Antarctica, Artic Ocean, Greenland
Characteristics = very cold, very dry, very stable

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4
Q

cP air mass

A

Continental polar = cP = high latitude plains of Eurasia + North America (Canada area)
Properties = cold, dry, very stable

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5
Q

mP air mass

A

maritime polar = mp = oceans in vicinity of 50-60 N/S latitude
properties = cold, moist, relatively unstable

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6
Q

cT air mass

A

continental tropical = cT = low-latitude deserts
Properties = hot, very dry, unstable

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7
Q

mT

A

Maritime Tropical = mT = tropical and subtropical oceans
Properties = warm, moist, often unstable

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8
Q

Front

A

meeting point btwn unlike air masses

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9
Q

Cold vs Warm front

A

Cold front = ADVANCING cold air mass meets + displaces warmer air

Warm Front = ADVANCING warm air mass meets + displaces COLDER air

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10
Q

Symbols for fronts

A

Cold = blue, triangles
Warm = red, semi-circles
stationary = combo of cold + warm
occluded = purple, trianges + semi-circles all pointing up

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11
Q

Characteristics of cold fronts

A

cold fronts steeper, move faster –> easily displaces lighter, warm air
effect = rapid lifting + adiabatic cooling of warm air, forming blustery, violent weather along front

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12
Q

warm front characteristics

A

gentler slope –> results in less turbulent weather + slower frontal uplift
broad precipitation, can become violent

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13
Q

stationary front

A

when neither air mass displaces other, “Stall”
gently rising warm air produces limited precip, long last stationary front could cause flooding
generally w. mT, cP

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14
Q

occluded front characteristics

A

cold front overtakes warm front
winter –> occluded associated w. blizzards
generally stable conditions for most occluded fronts

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15
Q

Midlatitude cyclones

A

associated w. air mass movement btwn 30-70 degrees
midlatitude’s = meeting point of tropical + polar fronts - leads to lots of storms

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16
Q

Characteristics of midlatitude cyclones

A

1) cold front extending to SOUTHWEST
2) warm front extending to NORTHEAST

SECTORS:
cool sector to north + west
warm sector to south + East

Cold front trailing + warm front leading

17
Q

Movement of midlatitude cyclone

A

1) travels along westerlies (ALL OF THEM GO TO EAST)
2) cyclonic wind circulation (Converges counterclockwise)
3) cold front moves faster than warm front
4) cold front moves south, warm front moves north

18
Q

Birth (Cyclogenesis of midlatitude cyclone)

A

cyclones start of as rossby waves in jet stream, when winds become meridonal (moving north/south) instead of zonal (West to east) chance of cyclone increases
cyclones need convergence below + divergence above to form properly

19
Q

what causes “death” of cyclone

A

Occlusion: eventually cold front overtakes warm front
as cold front catches up –> warm front is pushed further up until it is no longer in contact with earths surface –> occluded front formed
THIS means that short period of intensified precipitation + then low pressure center filled in, leaving the ground cooler + stable

20
Q

How does midlatitude cyclone change weather

A

temperature = cold front passes dropping temperature abruptly

pressure = pressure decreases as cold front passes + then increases steadily

wind = winds come from south (bc of counterclockwise spin) + once passes, winds shift and come from west/northwest

clouds/precip = cloudiness + precip at front, then turned to clear as adiabatic cooling of warm air occurs

21
Q

Midlatitude anticyclone

A

High pressure, moves west to esat bc of westerlies

22
Q

diff between midlatitude anticyclone + midlatitude cyclone

A

cyclones = have fronts + anticyclones have no fronts
anticyclones stall over region for several days while cyclones generally do not

23
Q

relationship btwn cyclones + anticyclones

A

1) generally alternate with one another
2) can occur independently BUT often have a functional relationship
**winds diverging from eastern part of anticyclone then go swooooooooosh into western side of cyclone (high to low pressure)