Weather Flashcards

(33 cards)

1
Q

Dew point

A

Air can’t hold any more moisture, saturated and begins to condensate
When water in air becomes visible as moisture, cloud, fog
Current temp more than 3 degrees from dew point to be safe

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2
Q

Atmosphere layers

A
Troposphere, up to 48k ft
Tropopause layer with Jetstream
Stratosphere 
Mesosphere
Thermosphere
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3
Q

Atmospheric circulation

A

Warm air rises at equator, moves up to poles, back down to equator

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4
Q

Atmospheric pressure

A

Decreases at one inch per 1000ft

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5
Q

Coriolis forces

A

Due to rotation of the earth
Northern hemisphere deflecting air to the right,eastward
Northeasterly trade winds from 30• to equator

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6
Q

Measuring atmospheric pressure

A

Aneroid vs mercurial barometer

Weather station pressure convertered to sea level, adding 1” Hg for every 1000ft

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7
Q

Currents and winds

A

Due to pressure differences, coriolis, friction, temperature differences
Upward, downward, horizontal
Cause weather changes

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8
Q

Cyclonic vs anti cyclonic circulation

A

Northern hemisphere high pressure deflection to the right clockwise pattern
Low pressure counterclockwise

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9
Q

High vs low pressure

A

High, descending dry air, good weather

Low, air flows into area to replace rising air, brings clouds, rain

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10
Q

Convective currents

A

Local circulation of air due to uneven heating of the ground, turbulence
Water, vegetation hearts slower

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11
Q

Low level wind shear

A

Dangerous

Due to passing frontal system, thunderstorms, temperature inversion, strong upper level wind

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12
Q

Microbursts

A
Servere type of low level wind shear 
Intense rain at the surface 
At cloud base ring of blowing dust 
1-2 miles diameter, depth of 1000ft
5-15min, downdrafts of up to 6000ft/min
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13
Q

Weather station symbols

A

Circle = station
Line points into direction where wind is coming from
Speed = barbs and pennants, 5, 10, 50

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14
Q

Isobars

A

Lines of equal pressure in mb
Close together = steep gradient, strong winds
Ridge = elongated area of high pressure
Trough = elongated area of low pressure

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15
Q

Adiabatic process

A

Heating and cooling off air when rising vs descending, temp lowers as air rises and expands
Moist air cools slower, rises higher, unstable

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16
Q

Inversion

A

Cool air below warmer air, at night, cool surface cools down few hundred feet of air, capped by top of layer

17
Q

How air can reach saturation point

A
  1. Warm air moves over cold surface
  2. Cold and warm air mix
  3. Air cools at night contact with cooler ground
  4. Air forced into high atmosphere
18
Q

Radiation vs advection fog

A

Ground cools rapidly, in valleys, air reaches dew point, vs

Wind pushes most warm air over cool surface, coastal fog

19
Q

Uplope vs steam vs ice fog

A

Wind pushes moist air up mountain range
Cold dry air moves over warm water causing water to evaporate
In arctic region, water vapor into ice

20
Q

Clouds

A

Air cools, reaches saturation point, deposition, sublimation, condensation, onto condensation nuclei (dust, salt, smoke)
Low - base up to 6500ft AGL
Middle - 6500-20k
High - above 20k

21
Q

Cloud classification

A
Cumulus
Stratus
Cirrus
Castellanus 
Lenticularus 
Nimbus
Fracto
Alto
22
Q

Ceiling

A

Lowest level of clouds reported as broken or overcast
Broken: 5/8 to 7/8 of sky covered
Overcast = 100% covered

23
Q

Cumulus clouds

A

Extensive vertical development
Base is low, extend high altitude
Instability, turbulence, thunderstorms
Lightning, hail, tornadoes, gusty, wind shear

24
Q

Precipitation

A

Drizzle, very small water droplets, fog
Virga, rain that evaporates before reaching the ground
Rain falling through temperature inversion may freeze, ice pellets

25
Air masses
Based on source region Take on surrounding characteristics Polar, tropical, dry deserts Moves over cold or warm land
26
Front
Boundary layer between 2 air masses, chances in weather imminent Warm, cold, stationary, occluded
27
Warm front
Slow moving, moves over cooler air, pushes it out, high humidity, fog, rain, thunderstorms when warm air is lifted, barometric pressure falling Stratiform clouds, cumulonimbus in summer
28
Cold front
Move rapidly, close to ground, forcing warm air up, forming clouds Cirriform, cumulus clouds, rain showers Can produce tornadoes, poor visibility, gusty winds, temperature and dew point dropping
29
Occluded front
Fast cold front catches up with slow warm front Cold front occlusion, mixture of weather Warm front occlusion, thunderstorms
30
Thunderstorm conditions
Air with sufficient water vapor, unstable lapse rate, initial lifting action Air mass storms (short) versus steady state storms (long)
31
Squall line
Narrow band of thunderstorms, ahead of cold front, moist unstable air, wide and long, forms rapidly
32
Tornado
Thunderstorm draw air into cloud with rotation, concentrated, 200kts winds, low pressure inside vortex, tornado of cloud touches ground, or waterspout, if water
33
Thundering hazards
``` Turbulence Icing Hail Ceiling and visibility Lightning Pressure Engine water ingestion ```