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

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8
Q

Anti-cyclone = high pressure

A
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9
Q

Coriolis least at equator, greatest at poles

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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

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13
Q

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

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14
Q

Trough = low
Ridge = high

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15
Q

Low = ascending air

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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

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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

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21
Q

Peak temp around noon
Min temp just after sunrise

22
Q

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

23
Q

Saturated air moving downhill temp warms slower

24
Q

Stability determined by lapse rate and cloud types

25
Variations of solar energy at Earth surface
26
Thermal low Dry, sunny region
27
Friction decreases wind speed and Coriolis force
28
Tropopause temp -55 to -65 (approx 2°/1,000 based on 36,000 avg tropopause)
29
Jet stream speed decrease greater on polar side
30
Large areas of land = increased temp variations
31
Coastal land surface cooling = land breeze
32
Stationary front = surface winds parallel front
33
Cold air = pressure increase
34
Winds parallel front = front moves slowly if any
35
Winds across front = rapid frontal movement
36
Frontal waves form in slow-moving cold or stationary fronts
37
Standard lapse rate 2°/1,000’ Unsaturated lapse rate 3°/1,000’ Saturated lapse rate 1°/1,000’
38
Water vapor to liquid = latent heat released
39
Dew point lapse rate / dry adiabatic lapse rate converge: Cloud bases form
40
Saturated air moving downhill = temp increase slower
41
Stability determined by cloud types
42
Clouds with extensive vertical development = unstable air
43
Cumulous clouds = possible turbulence
44
Haze is dispersed by wind
45
Wind above 15 knots lifts advection fog to create low stratus or stratocumulus layer
46
Moist air moving over rising ground = upslope fog
47
Warm rain/drizzle falling through cooler air = precipitation-i duced fog
48
Temp/dew point 10/10, light wind, clouds/rain = radiation fog
49
Lee side lake fog: warm air flowing over colder lake
50
Significant precip = min 4,000’ cloud thickness