NIFE Weather 6-2-2 Mechanics Flashcards

1
Q

2.185

Explain and identify gradient winds with respect to the isobars around pressure systems in the Northern Hemisphere.

A

Above 2000’ AGL

Shown via isobars - from high to lows

High pressure results from:

    • descending air
    • Creates horizontal diverging force (PGF)
    • flows clockwise

Low pressure results from:

  • Ascending air
    • Creates horizontal converging force (PGF)
    • counter-clockwise
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2
Q

2.186
Explain and identify the surface wind direction with respect to the gradient winds in a pressure system in the Northern Hemisphere

A

Pressure Gradient Force and Coriolis force balance to create flows.

    • Parallel to isobars.
    • Clockwise around Highs.
    • Counterclockwise around Lows.

Gradient winds.
- Found above 2,000 feet AGL.

Surface winds (below 2,000 feet AGL).

  • Friction reduces wind speed.
  • Coriolis force shifts wind direction toward isobars.
  • New balance of forces.
    • Wind blows across the isobars (45º).
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3
Q

2.187

Describe the jet stream

A

-A narrow band of strong winds 50kts or more that meanders vertically and horizontally around the hemisphere in wave-like patterns.

  • Ave height: 30000ft
  • 1000 to 3000 miles length
  • 100 to 400 miles width
  • 3000 to 7000 feet in depth
  • Average 100-150 knots
  • Flows West to East
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4
Q

2.188

Describe sea breezes

A
  • Onshore wind, blowing from the sea (cold air over water replaces warm air on land)
  • Day time
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5
Q

2.189

Describe land breezes

A

-At night cooler on land air moves over water producing wind moving offshore.

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6
Q

2.190

Define the term front

A

-An area of discontinuity that forms between two contrasting air masses when they are adjacent to each other
OR
-a border, boundary, or line between air masses

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7
Q

2.191

Describe the discontinuities used to locate and classify fronts

A

Temperature

  • Warm
  • Cold

Dew Point

  • Determines air mass boundary
  • larger contrast produces more severe weather

Pressure
- Falls ahead and rises after front passes

Wind
- Usually shifts 90* clockwise after front passes

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8
Q

2.192

Describe the characteristics of cold fronts

A
  • Leading edge of an advancing cold air mass.
  • Colder (denser) air mass is overtaking and wedging underneath a relatively warmer (less dense) air mass.
  • Unstable conditions
  • Moves SE at 20 knots
  • Wind switch from SW to from NW
  • Recognize by long line of cumulus clouds
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9
Q

2.192

Describe warm front

A
  • Boundary of the advancing warm air mass that is overtaking and replacing a colder air mass.
  • Warmer (less dense) air rides up and over the cold air mass
  • Stable Conditions
  • Moves NE at 15 Knots
  • Winds from SE shift to from SW
  • Recognize by straisform cloud and steady precip
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10
Q

2.192

Describe stationary fronts

A
  • Frontal border between the air masses shows little or no movement
  • Neither air mass is replacing the other
  • Shown by alternating cold warm front symbols and colors
  • 180* wind shift
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11
Q

2.192

Describe occluded front

A
  • Forms when a faster moving cold front overtakes a slower moving warm front
  • Either cold or warm depending on which stays in contact with surface
  • Winds shift 180*
  • Most severe weather location 100NM South to 300 NM North of intersection
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12
Q

2.193

Describe the characteristics of a squall line

A
  • A line of violent thunderstorms occurring in low pressure trough
  • Indicated by a dashed double dotted purple line.
  • Develop 50-300 miles ahead of a cold front and roughly parallel to it.
  • Worst in late afternoon/evening
  • 90 degree wind shift from SW to NW
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13
Q

2.194

Explain the relationship between flight conditions and atmospheric stability

A

FATVIPWC Chart

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14
Q

2.195

Describe the three characteristics of precipitation

A
  • Showers: Sudden beginning and ending/ cumuliform clouds
  • Continuous: Steady, intensity changes gradually/Stratiform Clouds
  • Intermittent: Stops and restarts at least once during the hour/associated with either cloud
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15
Q

2.196

Describe the cloud types

A
  • Low: Surface to 6500’ AGL
  • Middle: 6500’ to 20000’ AGL (alto-)
  • High: above 20000’ AGL (cirro-/cirrus-)

Cumuliform

  • lumpy, billowy cloud showing a definite pattern
  • Moist/Unstable air with showery precipitation (like Florida)

Stratiform:

  • Uniform base, horizontal sheet like layer
  • Moist/Stable air, constant precipitation (like Seattle)

Special:

  • Extensive vertical limits
  • nimbo/nimbus
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16
Q

2.199

Describe the four methods of lifting

A
  • Convergence: Two air masses force the air up
  • Orographic: Terrain lifts the wind (i.e. mountains, buildings)
  • Frontal: Cold fronts push warm air up
  • Thermal: Sun heats surface air causing it to rise
17
Q

2.2

Describe stability with respect to lifted air

A

Stability is determined by the temp of the surrounding air. If air returns to normal after lifting action, it is stable. If it continues to rise, it is unstable.

  • Stable: colder air settles when lifting action is removed
  • Unstable: Warmer air continues to rise after lifting action is removed
  • Neutral: Air of the same temperature remains at the point of where the lifting action was removed