Quiz 4 Flashcards

1
Q

air mass

A

large body with similar characteristics (T, moisture)

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2
Q

c, m, T, P, A, k, w

A

continental, marine, tropical, polar, arctic, unstable, stable

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3
Q

front

A

boundary between two air masses

named for one moving forward

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4
Q

signs of a cold front (5)

A
pressure drop at front (rising air)
decrease in dew point
drop in temp
shift in wind direction
cloud formation/precipitation
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5
Q

Cold front associated clouds (4)

A

cumulonimbus
cirrus
cirrostratus
altocumulus

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6
Q

signs of a warm front (5)

A
pressure drop at front (rising air)
increase in dew point
increase in temp
shift in wind direction
little precip
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7
Q

warm front associated clouds (5)

A
stratus
nimbostratus
altostratus
cirrostratus
cirrus
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8
Q

occluded front

A

cold front catches up to and overtakes a warm front; cold and warm type

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9
Q

3 stages of wave cyclone growth

A

cyclogenesis, open wave, advanced occlusion

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10
Q

cyclogenesis

A

high wind shear
circulation along stationary front
low pressure center forms at center of vortex

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11
Q

open wave

A

becomes mature when initial point of occlusion is reached

storm most intense at initial occlusion

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12
Q

advanced occlusion

A

cold front almost fully caught up to warm front

at triple point, secondary low pressure center forms

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13
Q

what does a midlatitude cyclone need to intensify?

A

must be an upper level trough (L) to the west of the surface low = divergence of air above surf low, strengthening system

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14
Q

baroclinic instability

A

positive feedback cycles that strengthen cyclone

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15
Q

baroclinic atmosphere

A

isotherms cross isobars
upper level wave will intensify
cold advection to the west will enhance sinking of air, intensifying surf H
warm advection to the east will cause rising air, causing surf L

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16
Q

barotropic atmosphere

A

isotherms parallel to isobars

no temp advection occurs

17
Q

ordinary vs severe Tstorms

A

ordinary: vertical updrafts
severe: slanted updrafts

18
Q

ordinary tstorms

A

most common

form in regions of low wind shear

19
Q

stages of ordinary Tstorm formation (3)

A

cumulus, mature, decaying

20
Q

Cumulus stage (ord tstorms)

A

updrafts dominate
water condenses
latent heat is released

21
Q

mature stage (ord tstorms)

A

appearance of downdraft
updrafts/downdrafts are vertical
gust front enhances updraft
strongest stage

22
Q

decaying stage (ordinary tstorms)

A

dominated by downdrafts

cuts off moisture source

23
Q

severe thunderstorms

A

vertical wind shear results in slanted updrafts and downdrafts
storms usually extend to tropopause

24
Q

supercell thunderstorm

A

updrafts are rotating

very high wind shear creates horizontal rotation, twisted into the vertical by updrafts

25
Q

squall line

A

Tstorms that form in front of a cold front

26
Q

tornado formation steps (5)

A
  1. high wind shear causes layer of air to roll (vortex tube)
  2. updrafts lift vortex tube into vertical orientation
  3. CCW cyclone survives, forming mesocyclone
  4. downdrafts in front and rear force air into mesocyclone, then air accelerates as moves closer (conserve ang mom)
  5. fast spinning air rises and diverges aloft, intensifying surf L –> increases surf convergence == positive feedback intensifies tornado
27
Q

lightning: charge separation (4)

A

hail collides with supercool liquid drops, drops freeze, releasing latent heat
warm hail collides with cold ice crystal, net transfer of + charge to crystal
+ ice crystals to top of storm, negative hail falls to bottom
also occurs when hailstorms are fragmented (smaller fragments carry + charge)

28
Q

lightning: electric potential

A

normally, earth has net negative charge compared to atmosphere (120V/m)
charge separation induces much greater positive charge on ground (200000V/m)

29
Q

lightning strike! (3.5)

A
  1. stepped leader: negative charge at base of cloud moves toward ground through air
  2. positive charges move upward to meet negative charge when close enough
  3. flash occurs when two streams meet, flow of positive ions is carried to cloud on return stroke

can be several pairs of strokes, returns per flash