FRONTS Flashcards

1
Q

Define Front

A

A transition zone between two air masses as it appears on the surface

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2
Q

Frontal surface

A

The sloping side of the cold air

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3
Q

What is the movement of the front dependent on?

A

The motion of the cold air that is perpendicular to it

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4
Q

The name of the front is always determined by:

A

The motion of its cold air

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5
Q

Types of fronts:

A

Cold front
Warm front
Occluded front
Trowal
Stationary front
Upper front

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6
Q

When does The transition zone (leading edge of a cold air mass) form?

A

When a wedge of cold air forces its way under a warm air mass called a frontal lift.

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7
Q

How fast can a cold front move

A

At speeds of 30 KT or more

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8
Q

Before a cold front passage
B.C
S,W,F,C,S,F,H
Some water flows cold some flows hot

A

Winds – beginning in the south to Southwest
Temperature – warm
Pressure – falling steadily
Clouds – increasing cumulus, towering cumulus, and cumulonimbus
Precipitation – short periods of showers
Visibility – fair to poor- haze
Dewpoint – high – remains steady

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9
Q

As cold front passes
D.C
G,D,R,CB,TS,P,D

A

Winds – gusting and veer and increase
Temperature – sudden drop
Pressure – sharp rise
Clouds – CB
Precipitation – formed by warm air, expanding as it is lifted by the advancing, cold air. Heavy rain, thunder and lightning, and maybe hail
Visibility – poor but improving
Dewpoint – sharp drop

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10
Q

After cold front passage
A.C
WDRWGL

A

Winds – becoming a West in Northwest
Temperature – steadily dropping
Pressure – rising steadily
Clouds, - slow, moving, warm air, stable, NS, AS, CI, fast, moving, warm, air, unstable, CU
Precipitation – showers, then clearing
Invisibility – good, except for in the showers
Dewpoint – lowering

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11
Q

Define warm fronts

A

A mass of warm air advances on a retreating mass of cold air. The warm air being lighter, ascends over the cold air in a long, gentle slope.

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12
Q

Before warm front passage
B.W

A

Winds – beginning in the south to Southwest
Temperature – cool to cold with slow warming
Pressure – falling gradually
Clouds – approaching in order: Sirus, cirrostratus, alto, stratus, Nimbo, stratus, stratus, and sometimes fog. CB in summer when fast moving and warm air is unstable TCU also likely when air is unstable.
Precipitation dash light to moderate: rain, snow, sleet, or drizzle
Visibility – poor
Dewpoint Dash steady rise

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13
Q

As a warm front passes
D.W

A

Winds– variable and veers
Temperature – steady rise
Pressure - levelling off
Clouds – stratus type, NS when there is precipitation
Precipitation – drizzle or none
Visibility – poor but improving
Dewpoint Dash steady

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14
Q

After warm front passage
A.W

A

Winds– becoming a south to south west
Temperature – warmer than steady
Pressure – slight rise, followed by fall
Clouds – clearing with scattered Strato cumulus SC, occasionally CB in summer
Precipitation – commonly none, sometimes light, rain, or showers
Visibility – fair in haze
Dewpoint – rise, then steady

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15
Q

Occluded front

A

This happens when a cold front associated with a low catches up to the warm front - over, taking it and undercutting the warm front

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16
Q

Trowal

A

In Canada, we use this for an inclusion trough wall is short for TRough Of Warm Air Aloft

17
Q

Add a Trowal (Occlusions) how many air masses are present?

A

3
A cold air mass
A cool, partially mixed air mass
A warm air mass aloft

18
Q

Stationary front

A

This is a front that is not moving, neither air mass is replacing the other. Wins will be blowing parallel to the front.

19
Q

Upper Fronts

A

A non-occlusion situation. These form when air is trapped on the surface, and the frontal weather is pushed aloft.

20
Q

Frontal fog
(precipitation fog)

A

This is a type of fog that is associated with weather at fronts, particularly warm fronts. This type of fog develops when frontal precipitation falls into the colder air a head of below the warm air, causing the cold air to become saturated through evaporation

21
Q

At what level is a front

A

Fronts in a GFA are drawn at the surface. Fronts on a SIGMET chart are also drawn according to their surface position.

22
Q

Stable frontal waves

A

Wind speeds typically are 15 to 20 kn, and can be up to 40 to 50 KT. It may last for two or three days.

23
Q

Frontogenesis:

A

is a meteorological process of tightening of horizontal temperature gradients to produce fronts.