Weather (11-16% of test) Flashcards

1
Q

Weather reports and forecasts can come from a FSS weather specialist. What is FSS?

A

Flight
Service
Station

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2
Q

What is the relation of “density altitude” and how does it effect aircraft?

A

Density altitude is the pressure of the atmosphere. As air pressure decreases, “density altitude” increases. In other words, “density altitude” increases with higher altitude.
A higher “density altitude” has lower atmospheric pressure which:
- Increases takeoff and landing distances because more air speed is needed around the air foil of a wing
- Decreases climb rates due to higher speeds needed for lift

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3
Q

What are the weather qualities of high pressure areas? (3)

A
  • Dry air
  • Descending air
  • Good weather
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4
Q

What are the weather qualities of low pressure areas? (4)

A

Low pressure generally means:

  • “bad weather”
  • cloudiness
  • precipitation (wet air)
  • ascending air
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5
Q

What are “convective currents”, what makes them, and how do they effect flight?

A

1) Convective currents are local air patterns close to the earth that change the direction of air flow.
2) Convective currents are caused by uneven solar heating of the ground. Barren land absorbs solar energy quickly this gives off more heat. Vegetated land and areas of waters absorbs solar energy slowly. This uneven heating causes currents of air movement.
3) Convective currents cause bumpy flights, turbulent air, updrafts over barren land, and downdrafts over water and vegetation.

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6
Q

Is air flow more turbulent on the Windward (side where wind is coming from)
or
Leeward side (backside of terrain relative to wind direction)?

A

Leeward

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7
Q

1) What is wind shear?
2) Why is it bad for aircraft?
3) What weather is low level windshear commonly associated with?
4) What is the most severe type of low – level windshear and ?

A

1) Sudden drastic wind speed changes.
Windshear is a sudden, drastic change in wind speed and/or direction over a very small area.
2) Updrafts, Downdrafts, and quick changes wind direction
Windshear can subject an aircraft to violent updrafts and downdrafts, as well as abrupt changes to the horizontal movement of the aircraft. A tailwind can quickly change into a headwind or vice versa.
3) Fronts, Storms, High winds
Watch out for frontal systems, thunderstorms, temperature inversions, and strong upper-level winds greater than 25 kn.
4) A Microburst.
“Microburst”, is associated with convective precipitation into a dry air and cloudbase. 

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8
Q

1) What is “dew point”?

2) Why is it important?

A

1) Temperature that air condenses moisture. Dew point, given in degrees, is the temperature at which the air can hold no more moisture and starts to condense.
2) Frost disrupts air flow over a wing and drastically reduced the production lift and increase drag. When air temps fall to the dew point fog, dew, frost, clouds, rain, or snow happens. If the temperature is below freezing = frost.
An aircraft must be thoroughly clean and free of frost prior to beginning the flight.

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9
Q

What are the 4 typical classifications of LOW cloud types?

A

Stratus, stratocumulus, nimbostratus, & fog

Strat means low: strat…, strat…c, n…strat, & fog

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10
Q

What type of clouds causes moderate icing?

A

Altostratus (mid-altitude long flat clouds)

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11
Q

1) What do cumulonimbus clouds cause?

2) What are they known as to pilots?

A

1) Bag Weather
Cumulonimbus clouds contain large amounts of moisture unstable air and usually produce hazardous weather phenomena, Such as lightning, hale, tornadoes, gusty winds, and windshear.

2) Most dangerous
To pilots, the cumulonimbus cloud is perhaps the most dangerous cloud types.

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12
Q

What are some conditions that define a stable air mass?

Air, Clouds, Precip., Visibility

A
  • Smooth air (not rough turbulence)
  • Stratiform thin clouds (not cumuliform) with no vertical development
  • CONTINUOUS precipitation (not showery)
  • Poor (to moderate) visibility (not good)
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13
Q

What are some of the conditions that define an UNstable air mass? (4)

(Air, Clouds, Precip., Visibility)

A
  • Rough turbulence (not Smooth air) or varying conditions
  • Cumuliform (Cumulus) clouds (not Stratiform) that build vertically is size
  • Showery precipitation (not Continuous) not consistent
  • Good visibility (not poor to moderate) caused by varying wind direction
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14
Q

1) What are the visual rules the remote PIC must adhere to before flight? (3)
2) What is the best way is to obtain local aviation report on visibility?

A
  • 3 statute miles (SM) visibility between sUAS and control station
  • 500 feet below clouds
  • 2,000 feet horizontally from all clouds
  • METAR (or TAF (if in controlled airspace)
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15
Q

Per the FAA what is the official FAA forecast of aviation activity for U.S. airports?

A

Terminal Area Forecast (TAF)

  • Cover the area 5 statue miles surrounding the airport
  • Only updated 4 times a day
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16
Q

What are the 5 parts of a Terminal aerodrome forecast (TAF) in order?

A

1) Type of Report
2) Station Identifier
3) Date & Time of Origin
4) Valid Period Start Date Time and End Date and Time
5) Forecast Condition: Wind, Visibility, Weather, Clouds. The repeating with each from = “FM”(2 digit date)(4 digit time)

17
Q

When should standard, abbreviated, or outlook briefings be requested (looked up)?

A

Standard - Prior to flight
Abbreviated - If flight is delayed
Outlook - Departure is 6 hours away

18
Q

What is sublimation?

A

Sublimation is the process that occurs when ice, is turned into water vapor.

19
Q

Describe “Radiation Fog”

A
Ground warm (radiating), Air cool and Wind calm. 
When sun heats ground all day, air is calm, then cool evening air come in. 
Radiation fog is a very common type of fog throughout the United States. It is most prevalent during the fall and winter. It forms overnight as the air near the ground cools and stabilizes. When this cooling causes the air to reach saturation, fog will form. Fog will first form at or near the surface, thickening as the air continues to cool. The layer of fog will also deepen overnight as the air above the initial fog layer also cools. As this air cools, the fog will extend upward.
20
Q

Describe “Advection Fog”.

A

Ground (water) cold, Air warm and moist, Wind do not have to be calm. (Beaches)
“Advection fog” forms as warmer, moist air moves over a cold ground.
The air is cooled to saturation by the cold from the ground below cooling the air above. Unlike radiation fog, advection fog may form under cloudy skies and with moderate to strong winds. Initial stability is relatively unimportant since low level cooling makes the air stable near the ground, allowing the fog to form. Once formed, it may move across the landscape, pushed by low level winds. Advection fog can last for several days and is most common in the U.S. on the West Coast.

21
Q

Describe “Upslope Fog”.

A

Upslope fog is formed when air flows upwards over rising terrain and is cooled to its saturation temperature.

22
Q

Describe “Steam Fog” or precipitation induced fog

A

Hot ground evaporated precipitation.
This typically happens during summertime in the ground has been heated by the sun all day and there is a slight shower precipitation that when it hits the hot ground immediately turns into steam.

23
Q

Describe cumulus low level clouds.

A

“Heap”

1) Cumulus: thick, white fluffy clouds that are scattered throughout the sky, building vertically.
2) Cumulonimbus: the Latin suffix “nimbus” means rain

24
Q

Describe stratus clouds.

A

Stratus = layer

Stratus clouds are typically dismal clouds that fill the sky with a layer of dark cover. 

25
Q

Describe cirrus clouds. 

A
  • High level
  • Classified as 20,000 feet and above. 
  • Wispy and thin
  • Indicate change in weather
26
Q

What is the 2nd most intense stage of a thunderstorm?

A

Mature Stage