7.Pressure & Wind Flashcards

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1
Q

define pressure

A

• a force exerted over a given surface area is pressure

  • air molecules are pulled down toward Earth’s surface by gravity
  • because these molecules are moving, they exert a force on anything they are in contact with
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2
Q

1000 Pa=__kpa=__mb

A

1, 10

-all units of pressure

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3
Q

Newtons 2nd law of Motion:

force= ____ x _____

A

mass x acceleration

• if 2 objects accelerate at the same rate, the heavier object will require more force to keep up
• we must also consider all of the forces, including the forces pushing the object and the forces resisting the motion of the forces
-vertical winds try and counter gravit

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4
Q

The pressure at Earths surface is on average ______ mb

A

1013.2

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5
Q

T OR F

pressure is proportional to the rate of collision between the molecules and a surface

A

T

• an increase in pressure implies that there is a greater rate of collision, while a decrease in pressure implies fewer collisions

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6
Q

2 ways to increase rate of collisions, and therefore pressure

A
  1. increase the density (add molecules, or decrease the volume) 2. raise the temperature (ie, the speed of the molecules
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7
Q

Partial Pressure

A

a specific pressure that different molecules inidividually have based on Molar Mass

  • C02 very high
  • sum of all partial pressures is the total pressure
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8
Q

Vertical Pressure Gradient

A
  • counters gravity in that it makes molecules want to rise because they always want to go from high to low pressure in upper atmos
  • ex: air baloons expanding tremendously at high altitudes
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9
Q

You always need to correct pressure measurements for _____

A

altitude

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10
Q

roughly,pressure decrease by __ mb for every 10 m you ascend

A

1

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11
Q

_____plays a much larger role in pressure then temperature does

A

density

  • although not contained in the ideal gas law water content also has an effect on air density
  • really really humid days, air is actually lighter compared to dry days
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12
Q

Does Dry or wet air create more pressure?

A
  • dry air (ie, containing no water) has an average molecular weight of 28.5
  • H2O has a molecular weight of 18.01, so as water content in the air (ie, humidity) increases, the molecular weight of the atmosphere decreases, and pressure decreases
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13
Q

• the standard instrument for measuring atmospheric pressure is the ________ ________

A

mercury barometer

-• Hg is used because of its high density – if water were used, the barometer would have to be 10m tall

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14
Q

3 corrections have to be made to barometer readings for them to be accurate:

A
  1. Compensation for elevation
  2. Compensation for temperature
    - as temperature increases, Hg expands (and vice versa) which can be mistaken for a change in pressure
  3. compensation for gravity
    - acceleration due to gravity is greater at higher latitudes

• we therefore describe barometric pressure as being relative to sea level, 0 °C, and at 45 °N

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15
Q

aneroid barometer

A

-much cheaper option
• air pressure collapses a chamber, and the attached needle reflects this change on a scale
• each aneroid barometer is calibrated to the specific location, so it automatically accounts for elevation and gravity
– temperature is irrelevant, since there is no expandable fluid in it

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16
Q

isobars

A

lines of equal pressure

17
Q

Using isobars we can determine the pressure _____

A

gradient

18
Q

________ causes wind to blow

A

pressure gradient

  • if the pressure gradient is strong, then the isobars are close together, the pressure difference is great, and wind speed is hgih
  • if the pressure gradient is weak, then the isobars are far apart, the pressure difference is small, and wind speed is low
19
Q

Horizontal Pressure Gradient

A

• across Earth’s surface, pressure is often distributed as series of high and low pressure centres, with winds blowing between them from high to low • the typical pressure difference though is very small – low pressure is typically 980 mb while high pressure is typically 1020 mb; a difference of only 40 mb • the distance separating these high and low centres can be very large, on the order of 3000 km • this produces a relatively weak average horizontal pressure gradient of 1 mb per 75 km • sometimes, this pressure gradient can become much greater • the pressure gradient between the centre of a hurricane and the outer edge can be as much as 1 mb per 6 km

20
Q

• the typical pressure difference though is very small – low pressure is typically ___ mb while high pressure is typically ___ mb; a difference of only 40 mb

A

980

1020

21
Q

Vertical Pressure Gradients

A

-vertical pressure gradients are much greater than horizontal pressure gradients
• average sea level pressure is 1013.2 mb while at 500m up it is 500 mb, a pressure gradient of about 1 mb per 10 m
• compare this to the relatively strong horizontal gradient of a hurricane at 1 mb per 6 km
• if vertical pressure gradients are so much greater than horizontal gradients, why do we consider wind to be a horizontal process

22
Q

Why do we think of wind being a horizontal proccess?

A
  • although air would prefer to flow upwards, gravity is pulling it back down to the surface
  • vertical pressure gradient is balanced by the pull of gravity
23
Q

there is a greater vertical pressure gradient through ______ air because of higher density

A

colder

24
Q

Coriolis Force

A

to the right in north, left in south

25
Q

Coriolis is dependent solely on

A

wind speed

26
Q

4 important facts about coriolis

A
  1. the Coriolis force produces an apparent deflection in all moving objects, regardless of their direction of motion (deflection is to the right in the Northern Hemisphere and to the left in the Southern Hemisphere)
  2. the Coriolis force is zero at the equator and increases with increasing latitude, reaching a maximum at the poles
  3. the Coriolis force acting on any object increases with the object’s speed
  4. the coriolis force changes only the direction of a moving object, never its speed
27
Q

2 layers of earths atmosphere in terms of friction=

A
  1. Planetary Boundary Layer <1.5 km
    - friction

2.Free atmos
>1.5 km
-almost non existant friction

28
Q

3 forces that effect wind speed and direction

A
  1. Pressure Gradient= +
  2. Coriolis effect= minor
  3. Friction= -
29
Q

If earth didnt rotate winds would flow …

A

northward following upper atmos pressure surface

30
Q

Geostrophic flow/wind

A

-upper air movement caused by balance of pressure gradient and coriolis causing eastward flowing wind in North
• geostrophic flow is very stable, and is not easily disrupted
• eg, an increase in the pressure gradient would cause the wind to shift northward, but the associated increase in windspeed would enhance the Coriolis force, bringing the flow back to eastward