Weather Flashcards

1
Q

How does the air flow in regard to high or low pressure systems in the northern hemisphere

A

High pressure - outward, downward, clockwise

Low pressure - inward, upward, counterclockwise

PHAK 12-7

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2
Q

What kind of weather can you expect in a low-pressure system versus a high-pressure system.

A

Low pressure system - characterized by rising air, which is conductive to cloudiness, precipitation and bad weather.

High-pressure system - characterized by descending air which tends to favor dissipation of cloudiness and good weather.

PHAK 12-7

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3
Q

Describe the different types of fronts.

A

Cold - occurs when a mass of cold dense, and stable air advances and replaces a body of warmer air.

Occluded - occurs when a fast-moving cold front catches up with a slow-moving warm front. Two-types: cold front occlusion and warm front occlusion

Warm - The boundary area formed when a warm air mass contacts and flows over a colder air mass.

Stationary - When the forces of two air masses are relatively equal, the boundary or front that separates them remains stationary and influences the local weather for days. The weather is typically a mixture of both warm and cold fronts.

PHAK 12-18

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4
Q

What kind of weather can you expect in a cold front versus a warm front?

A

Cold - As the front passes, expected weather can include towering cumulus (intermediate) or cumulonimbus (intense), heavy rain accompanied by lighting, thunder and/or hail; tornadoes possible; during passage poor visibility, winds variable and gusting; temperature/dew point and barometric pressure drop rapidly.

Warm - As the front passes, expected weather can include stratiform clouds, drizzle, low ceilings and poor visibility; variable winds; rise in temperature

Note: the weather associated with a front depends on the amount of moisture available, the degree of stability of the air that is forces upward, the slope of the front, the speed of frontal movement, and the upper wind flow.

PHAK 12-18

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5
Q

What is a trough

A

An elongated area of low pressure system

PHAK 12-12

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6
Q

What is a ridge

A

An elongated are of high pressure system

PHAK 12-12

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7
Q

What are the standard temperature and pressure values for sea level

A

59 °F or 15 °C and a surface pressure of 29.92 inches of mercury (“Hg) or 1,013.2 mb

PHAK 4-3

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8
Q

What are isobars

A

Isobars are lines drawn on a weather chart to depict lines of equal pressure.

PHAK 12-12

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9
Q

What happens if the isobars are relatively close together versus widely spaced.

A

Close together - a steep pressure gradient exists which indicates higher wind speeds.

Widely spaced - a shallow pressure gradient usually means wind speeds will be less.

PHAK 12-12

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10
Q

What causes the winds aloft to flow parallels to the isobars.

A

Coriolis force.

PHAK 12-4

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11
Q

Why fo surface winds generally flow across the isobars at an angle.

A

Surface friction.

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12
Q

At what rate does the atmospheric pressure decrease with an increase in altitude.

A

Standard pressure lapse rate is 1” Hg per 1000 feet.

PHAK 4-3

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13
Q

What does “dew point” mean.

A

The temperature to which a sample of air must be cooled to attain the state of saturation.

When the temperature of the air is reduced to the dew point, the air is completely saturated and visible moisture begins to condense out of the air in the form of fog, dew, frost, clouds, rain, or snow

PAHK 12-13

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14
Q

What factor primarily determines the type and vertical extent of clouds.

A

The stability of the atmosphere.

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15
Q

What is the difference between a stable atmosphere and an unstable atmosphere. Why is the stability of the atmosphere important.

A

The stability of the atmosphere depends on its ability to resist vertical motion. A stable atmosphere makes vertical movement difficult, and small vertical disturbances dampen out and disappear.

In an unstable atmosphere, small vertical air movements tend to become larger, resulting in turbulent airflow and convective activity.

Instability can lead to significant turbulence, extensive vertical clouds, and severe weather.

PHAK 12-12

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16
Q

List the effects of stable and unstable air.

A

STABLE UNSTABLE

Clouds Stratiform Cumuliform
Turbulence Smooth Rough
Precipitation Steady Showery
Visibility Fair to poor Good

PHAK 12-12

17
Q

What type of weather information should you be aware with respect to icing when preflight planning?

A
  • Location of fronts, type speed and direction of movement
  • Cloud layers, location of cloud bases and tops (PIREPS and area forecasts)
  • Freezing levels, to avoid icing and how to exit icing conditions
  • Air temperature and pressure, icing tends to be found in low-pressure areas and at temperatures at or around freezing.
18
Q

What is freezing level and where can it be found.

A

The lowest altitude in the atmosphere over a given location at which the air temperature reaches 0°C. Can be found on freezing level graphic chart, PIREPs, AIRMETs, SIGMETs, surface analysis charts, low-level significant weather charts, and winds and temps aloft.

It is possible to have multiple freezing levels when a temperature inversion occurs above the defined freezing level.

19
Q

What conditions are necessary for structural icing to occur.

A

Visible moisture and below freezing temperatures at the point moisture strikes the aircraft.

20
Q

Name the main types of icing an aircraft may encounter in-flight.

A

Structural (on the wings), induction system (carburetor), and instrument icing (pitot head)

21
Q

Name the three types of structural icing that may occur in flight.

A

Clear ice -Glossy, clear, or translucent ice formed by the relatively slow freezing of large, supercooled water droplets.

Rime ice - Rough, milky, opaque ice formed by the instantaneous freezing of small supercooled water droplets.

Mixed ice - A mixture of clear and rime ice.

22
Q

What should you do if you inadvertently encounter icing conditions in-flight.

A

Turn around and leave the area of visible moisture. Descend to an altitude below the cloud bases and where the temperature is warmer.

23
Q

Is frost consider to be hazardous to flight, why?

A

Yes, frost disrupts the smooth flow of the air around the wings, thus causing a separation of airflow and resulting in lost of lift.

24
Q

What factors must be present for a thunderstorm to form.

A

Unstable air, lifting action, moisture.

25
Q

What are the three stages of a thunderstorm

A

Cumulus - updrafts cause raindrops to increase in size.

Mature - Rain at earth’s surface; it falls through or immediately beside the updrafts; lightning; perhaps roll clouds

Dissipating stage - Downdrafts and rain begin to dissipate.

26
Q

What is a temperature inversion.

A

An increase in temperature with increase in altitude. An inversion aloft permits warm rain to fall through cold air which can be critical to icing. A ground-based inversion favors poor visibility by trapping fog, smoke, and other restrictions.

27
Q

State two basic ways that fog may form

A
  • When the temperature and dew point meet.

- Adding moisture to the air near the ground.

28
Q

Name several types of fog

A

Ice fog - occurs in cold weather when the temperature is much below freezing and water vapor forms directly into ice crystals

Steam fog - forms when cold, dry air moves over warm water

Upslope fog - occurs when moist, stable air is forced up sloping land features like a mountain range

Precipitation fog

Radiation fog - On clear nights, with relatively little to no wind present. Occurs when the ground cools rapidly due to terrestrial radiation, and the surrounding air temperature reaches its dew point. As the sun rises and the temperature increases,
radiation fog lifts and eventually burns off. Any increase in wind also speeds the dissipation of radiation fog.

Advection fog - When a layer of warm, moist air moves over a cold surface or water. Unlike advection fog, it may occur with winds, cloudy skies, and at any time of the day or night.

PHAK 12-15

29
Q

Define wind shear and state the areas in which it is likely to occur.

A

A sudden change in wind direction and velocity. It may occur with a low-level temperature inversion, in a frontal zone or thunderstorm and at high levels associated with a jet stream (clear air turbulence).

PHAK 12-11

30
Q

What types of weather information will you examine to determine if wind shear conditions might affect your flight.

A

Any mention or indication of severe thunderstorms, heavy rain, warming trends, gusty winds, cumulonimbus clouds, hail, etc. Suggests the potential for low level windshear and microbursts.

TAFs, METARs, convective SIGMETS, LLWAS (low level windshear alert system) and PIREPS

31
Q

What is the primary means of obtaining a weather briefing.

A

The flight service station (FSS), 1800-WX-BRIEF and the 1800WXBRIEF.COM

FAR 7-1-2

32
Q

What types of weather briefings are available from anAFSS/FSS briefer.

A

Standard - when planning a flight and you have not received a previous brief

Abbreviated - when you need to update a previous brief, or you need one or two items

Outlook - when your proposed time of departure is six or more hours ahead

Inflight - when needed to update a preflight briefing

FAR 7-1-5

33
Q

What pertinent information should a weather briefing include.

A
  • Adverse conditions
  • VFR flight not recommended
  • Synopsis
  • Current conditions
  • Enroute forecast
  • Destination forecast
  • Winds aloft
  • NOTAMs
  • ATC delays
  • Pilot may obtain information regarding special use airspace; alert areas, MOA, MTRs (IR, VR, SR), warning areas and assigned airspace.

FAR 7-1-5

34
Q

What is a HIWAS.

A

Hazardous in-flight weather advisory service is a continuous broadcast of weather advisories including summarized aviation weather warnings,
SIGMETs, Convective SIGMETs, Center weather advisories, AIRMETs, and urgent PIREPs.

FAR 7-1-10