Chapter 3 - Atmospheric Pressure and Winds Flashcards

1
Q

The weight of column of air at a given place and time is called ________

A

Pressure

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2
Q

The international standard pressure unit is the ________

A

Pascal

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3
Q

The mean atmospheric pressure at sea level is ________

A

1013.25 mb

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4
Q

The columnar distribution of atmospheric pressure is known as

A

Vertical distribution of pressure gradient

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5
Q

The normal rate of decrease in air pressure is ________

A

34 mb/ 300 m

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6
Q

The distribution of atmospheric pressure over the globe is known as ________

A

Horizontal distribution of pressure

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7
Q

The ratio between pressure difference and the actual horizontal distance between the two points.

A

Pressure gradient

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8
Q

This belt is also known as the doldrums (the zone of calm) due to virtual absence of surface winds

A

Equatorial Low Pressure Belts

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9
Q

a.k.a ITCZ

A

Equatorial low pressure belt

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10
Q

the existence of these pressure belts is due to the fact that the rising air of the equatorial region is deflected towards pole due to the earth’s rotation

A

sub-tropical high pressure belts

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11
Q

The worldwide system of winds is called

A

General Atmospheric Circulation

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12
Q

Horizontal movement of air is in response to difference in pressure is termed as _______

A

Wind

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13
Q

Describes the pattern of deflection taken by objects not firmly connected to the ground as it travel long distances around and above the earth

A

Coriolis Effect

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14
Q

This cell creates some of the most important weather patterns on earth. As air rises and travels northward to the east, it eventually falls around 30. Where this air descends, it creates a ring of high atmospheric pressure

A

Hadley Cell

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15
Q

In this cell, air converges at low altitude or ascends along the boundaries between polar air and the warm subtropical air

A

Ferrel Cell

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16
Q

air sinks over the highest latitudes and flows out towards the lower latitudes at the surface

A

Polar Cells

17
Q

This type of wind blows from high pressure belts to low pressure belts in the same direction throughout the year

A

Planetary wins

18
Q

The winds that move poleward from subtropical high pressure in the northern hemisphere are deflected to the right and this blow from the south west.

A

Westerly

19
Q

The winds that blow from sub-tropical high pressure areas towards equatorial low pressure areas

A

Easterly

20
Q

This wind blow from polar regions towards sub-polar low pressure regions

A

Polar easterly

21
Q

The direction of these winds changes with the season

A

Periodic Winds

22
Q

A seasonal change in the direction of the prevailing, or strongest winds of a region

A

Monsoon Winds

23
Q

This type of winds is caused by the differences in air temperature. The temperature differences often develop through the sun

A

Local Winds

24
Q

Any wind characterized by intense heat and low relative humidity

A

Hot winds

25
Q

Wind which may blow very strongly over the northern plains of India and Pakistan in the months of May and June

A

Loo

26
Q

Warm, dry, downslope wind that descends on the eastern slope of the Rocky mountains. Strong westerlies aloft flow over a north-south trending mountain range,

A

Chinook

27
Q

Strong, dusty warm local wind which develops on the leeward side of the alps mountain ranges

A

Foehn

28
Q

The local winds that originate in the snow-capped mountains during winter and move down the slopes towards the valleys

A

Cold Winds

29
Q

The most common local winds and originate on the Alps and more over France towards the Mediterranean Sea through Rough Valley. They are very cold, dry and high velocity winds

A

Mistral

30
Q

A line connecting points that have equal values of pressure

A

Isobars

31
Q

Change in pressure is referred to as

A

Pressure Gradient