Chapter Six - Test Three Flashcards

1
Q

Although pressure is the “least sensible” of the six weather elements we examine in this class, its role in meteorology is vital because:

A
  • Spatial variation of pressure generates wind
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2
Q

Wind is responsible for

A

advection of temperature and moisture

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3
Q

Air Pressure [p]:

A

the force (per unit area) exerted by the weight of a column of air above a given point
- the force is created by the continuous
collision of gas molecules (N2, O2, Ar…)

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4
Q

At mean sea level (msl), the average p is:

A
  • 14.7 ibs in^-2
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5
Q

Measuring Air Pressure

Meteorological applications do not use lbs in-2; rather we use:

A

Inches of mercury (in Hg): reported to the public

  • Millibars (mbs): used by meteorologists
    1. 0 lbs in-2 = 2.04 in Hg = 68.9 mbs
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6
Q

At msl the average pressure equals:

A

14.7 lbs in-2 = 1013.25 mb = 29.92 inches Hg

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7
Q

Typical values and ranges of barometric pressure (mbs, in Hg) observed at mean sea level

A

Highest ever: 32.01 in Hg

Lowest ever: 25.70 in Hg

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8
Q

Instruments used to measure air pressure are called:

A

Barometers- Instruments that measure “bars”

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9
Q

Since we measure pressure with barometers, we refer to it as:

A

Barometric Pressure

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10
Q

The first barometer was invented in ____ by ____ and is very similar to liquid barometers still used today.

A

1643, Torricelli

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11
Q

Mercury barometer:

A

a column of mercury in a glass tube is in balance with the weight of the air above it.
Advantages: very accurate
Disadvantages: expensive mercury is toxic

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12
Q

Why use Hg in a barometer, especially if it’s a toxin?

A

Any liquid could be used, such as water. But, since water is much less (13.6x) dense than Hg, the height of the barometer would have to be much greater (13.6x)!
So: a typical barometric pressure of 30.00” Hg would equal 408.0” water (34’)…….
Necessitating a very large instrument!

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13
Q

Aneroid Barometer:

A

consists of a small metal “box” called an aneroid (w/o liquid) cell that has had some of its air removed before sealing

An increase (decrease) in pressure cause the box to contract (expand)

This “signal” is then amplified with levels.
Advantages: relatively inexpensive, contains no toxic liquid, most common home barometer
Disadvantages: needs frequent calibration

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14
Q

Two variations of aneroid barometers are :

A

Barograph & Pressure Altimeter

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15
Q

Pressure Altimeter:

A

an aneroid barometer labeled to indicate altitude (instead of barometric pressure)
- used in aircraft

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16
Q

Barograph:

A

a recording aneroid barometer that uses strip charts and timing mechanism (Fig. 6.5)
- provides trend information

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17
Q

Pressure ____ very rapidly wrt altitude

A

decreases; (∆p/ ∆z) is much less than 0

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18
Q

In the troposphere, where the decrease is linear, we can approximate the lapse rate using:

A

(∆p/ ∆z) = (-1 mb/10 meters)

Due to this rapid change, even a small difference in elevation between two surface observations can result in a large, misleading difference in barometric pressure.

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19
Q

To compensate for different station elevations, we make: Elevation corrections

so that all station pressures are adjusted to an altitude of 0 meters (msl) which we call:

A

Equivalent Sea Level Pressure (ESLP)

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20
Q

Station Station Pressure Elevation
A 1008 mb 0 m
B 915 mb 1000 m
C 840 mb 1800 m

A

ESLP
1008+ 0= 1008 mb
915+100 = 1015 mb
840+ 180 = 1020 mb

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21
Q

Horizontal Variations in Air Pressure

After making the corrections to equivalent sea level pressures, we then plot the values on a map and then analyze the horizontal variations using:

A

Isobars: lines of equal pressure

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22
Q

Isobars allow us to…

A

locate areas of high and low pressure, and strong and weak pressure differences.

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23
Q

Wind:

A

nature’s attempt to balance inequalities in air pressure which are due to inequalities in surface heating

24
Q

In order to determine wind direction and speed, we must identify all of the influencing forces

A

1) Pressure Gradient Force (Fpg)
2) Coriolis Force (Fco)
3) Frictional Force (Ff)

25
Q

Pressure Gradient Force (Fpg)

A

This Force results from differences in pressure represented by pressure gradients (Fig 6.9, 6.10)

The Fpg is this force that causes the air to move (wind)

26
Q

The Fpg is this force that causes the air to move (wind)

A

It is directed from high pressure to low pressure at right angles to the isobars
- its magnitude is directly proportional to the pressure gradient

27
Q

closely spaced isobars indicate:

A

Strong gradient, high winds

28
Q

widely spaced isobars indicate:

A

Weak gradient, light winds

29
Q

If the FPG was the only force acting on the atmosphere, the wind would blow directly from areas of…

A

high pressure to areas of low pressure; however, the instant the air starts moving, its path (direction) is deflected by the: Coriolis Force (Fco)

30
Q

The Fco is an apparent force due to earth’s rotation

A

all free moving objects (planes, projectiles, air) seem or appear to deflect from a straight-line path because the earth rotates underneath them (Fig 6.12; 6.13)

  • impacts wind direction only, not wind speed
  • in the NH the wind is deflected to the right
31
Q

The magnitude of the FCO depends on:

A

1) rotation rate of the earth (Omega)
2) Latitude (O mega)
3) Speed of the wind (V)

32
Q

Fco can be calculated using:

A

Fco = 2 x V x Ω x sin (latitude)
Where V = wind speed and…
Ω = 360º/ 24 hours = 7.29 x 10 -5 s-1

33
Q

We can see from the Fco equation, that:

A
  • The stronger the wind, the greater the Fco
  • The higher the latitude, the greater the Fco
  • At the equator (0 ), Fco = 0
  • At the poles (90), Fco is maximum (for a given V)
34
Q

Note that under any conditions Fco is a very small force, and subsequently only comes into play when considering large time and space scales…

A

therefore it does not influence water going down drains!

35
Q

Within ~ 1500 meters of the surface, an area we call the Friction Layer. A third force, called the ____ must be considered.

A

Friction Force (Ff)

36
Q

The Friction force (Ff) is dependent on:

A
  • Height: as you near the surface, the Ff maximizes (fig. 6.14a)
  • Surface roughness: the rougher the terrain (i.e. mountains) the stronger the Ff
37
Q

Above the Friction Layer (where FF = 0) Fig. 6.15 illustrates that the FPG and the FCO evolve into a balanced scenario resulting a wind called the:

A

Geostrophic Wind (Vg)

38
Q

The direction of the Vg is always

A

parallel to the isobars, with its speed proportional to the gradient of the isobars.

39
Q

Using Buys-Ballot’s Law, we can see that if you stand with your back to the wind (in the NH), the Vg blows with:

A
  • Low pressure on your left

- High pressure on your right

40
Q

In Geostrophic wind examples…
Fco-
Vg-
Fpg-

A

Fco - always directed 90º to the right of the wind
Vg- always parallel to the isobars
Fpg- always directed from high to low pressure at right angles to the isobars

41
Q

An aloft high pressure center has what characteristics?

A
  • Clockwise (Anticyclone) Circulation

- Parallel Flow

42
Q

An aloft low pressure center has what characteristics?

A
  • Counterclockwise (Cyclonic) Circulation

- Parallel Flow

43
Q

Within the Friction Layer (less than 1500 m) we must take into account the Ff

A
  • reduces the wind speed, which in turn

- reduces the Fco (which is a function of velocity)

44
Q

Since the FCO is reduced in the Friction Layer, it can no longer balance the FPG; as a result the wind within the friction layer flows:

A
  • At a reduce speed

- Across the isobars, toward low pressure

45
Q

Surface Winds

The average angle at which the wind crosses the isobars at the surface:

A
  • 30 degrees

but it can vary depending upon the surface roughness and range from:

  • 10 degrees over the oceans,
  • 45 degrees over mountains
46
Q
In Surface wind examples...
Fco-
Ff-
Fpg-
V-
A

Fco- always directed 90º to the right of the wind
Ff- always directed in the opposite direction of the wind
Fpg- always directed from high to low pressure at right angles to the isobars
V- cross isobar flow towards low pressure

47
Q

A surface high pressure center has what characteristics?

A
  • Clockwise (Anticyclone) outflow

- Surface Divergence

48
Q

A surface low pressure center has what characteristics?

A
  • Counterclockwise (Cyclonic) inflow

- Surface Convergence

49
Q

Although the vertical transport of air is generally much ____ than the horizontal transport, it is nonetheless critical to most of what we consider weather (Fig 6.22).

A

slower

50
Q

Surface winds associated with a Cyclone:

A

Converge toward the center.

Since the converging air can’t go into the ground it must rise, thereby:
Producing clouds and precipitation

51
Q

Surface Winds associated with an Anticyclone:

A

Diverge from the center.

To replace the laterally diverging air, air aloft must sink, thereby:
Inhibiting clouds and precipitation.

52
Q

Meteorologists measure and report wind:

A

speed : { ms. -1, mph, knots}

direction : (FROM which it blows) {degrees, quadrants. (i.e. nw, se)

53
Q

Wind measurement instruments include:

A

Wind Vanes: measure direction
Cup Anemometers: measures speed
Aerovane: measures speed and direction

54
Q

Wind Roses

A

provide a method of representing prevailing winds by indicating the % of times the wind blows from a particular direction.

55
Q

Prevailing winds from RDU are coming from the ____ direction

A

southwest