AVWX Flashcards

1
Q

Break in tropopause

A
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2
Q

Cirrus on equatorial side

A
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3
Q

Wind shear on polar side of jet stream due to greater wind speed decrease

A
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4
Q

Large land masses = increase temp variations

A
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5
Q

Tropopause:
abrupt change lapse rate
Decrease temp w increase altitude

A
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6
Q

Arctic and subtropical wx system movement:
East to west

A
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7
Q

Indian Ocean

A
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8
Q

Anti-cyclone = high pressure

A
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9
Q

Coriolis least at equator, greatest at poles

A
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10
Q

Occluded front crossed by jet stream

A
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11
Q

Jet stream
50 knots or greater
Winter = strongest
Occluded front
North of surface wx systems

A
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12
Q

Steep frontal surface = cold front

A
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13
Q

Dew point front (dry line):
Air density and dew point difference

A
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14
Q

Trough = low
Ridge = high

A
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15
Q

Low = ascending air

A
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16
Q

Parcel of air colder than surrounding air will sink

A
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17
Q

Frontal waves form in slow-moving cold fronts or stationary fronts

A
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18
Q

Katabatic = downsloping wind

A
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19
Q

Adiabatic = temp change by expansion or compression

Expansion = cooling
Compression = warming

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20
Q

Cloud bases form

A
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21
Q

Peak temp around noon
Min temp just after sunrise

A
22
Q

Inversion:
Stable air
Poor visibility
Wind shear
Clear, calm night

A
23
Q

Saturated air moving downhill temp warms slower

A
24
Q

Stability determined by lapse rate and cloud types

A
25
Q

Variations of solar energy at Earth surface

A
26
Q

Thermal low Dry, sunny region

A
27
Q

Friction decreases wind speed and Coriolis force

A
28
Q

Tropopause temp -55 to -65
(approx 2°/1,000 based on 36,000 avg tropopause)

A
29
Q

Jet stream speed decrease greater on polar side

A
30
Q

Large areas of land = increased temp variations

A
31
Q

Coastal land surface cooling = land breeze

A
32
Q

Stationary front = surface winds parallel front

A
33
Q

Cold air = pressure increase

A
34
Q

Winds parallel front = front moves slowly if any

A
35
Q

Winds across front = rapid frontal movement

A
36
Q

Frontal waves form in slow-moving cold or stationary fronts

A
37
Q

Standard lapse rate 2°/1,000’
Unsaturated lapse rate 3°/1,000’
Saturated lapse rate 1°/1,000’

A
38
Q

Water vapor to liquid = latent heat released

A
39
Q

Dew point lapse rate / dry adiabatic lapse rate converge:
Cloud bases form

A
40
Q

Saturated air moving downhill = temp increase slower

A
41
Q

Stability determined by cloud types

A
42
Q

Clouds with extensive vertical development = unstable air

A
43
Q

Cumulous clouds = possible turbulence

A
44
Q

Haze is dispersed by wind

A
45
Q

Wind above 15 knots lifts advection fog to create low stratus or stratocumulus layer

A
46
Q

Moist air moving over rising ground = upslope fog

A
47
Q

Warm rain/drizzle falling through cooler air = precipitation-i duced fog

A
48
Q

Temp/dew point 10/10, light wind, clouds/rain = radiation fog

A
49
Q

Lee side lake fog: warm air flowing over colder lake

A
50
Q

Significant precip = min 4,000’ cloud thickness

A