Ch. 5 Flashcards

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1
Q

atmospheric pressure

A

the force exerted by the weight of these gas molecules on a unit of area of earths surface or any other body

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2
Q

temp and pressure relationships

A

an increase in temp creates a decrease in density and thus a decrease in pressure and vise versa

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3
Q

dynamic high

A

strongly descending air is usually associated with high pressure at the surface

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4
Q

thermal high

A

very cold surface conditions are often associated with high pressure at the surface

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5
Q

dynamic low

A

strongly rising air is usually associated with low pressure at the surface

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6
Q

thermal low

A

very warm surface conditions are often associated with relatively low pressure at the surface

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7
Q

barometers

A

measure atmospheric pressure

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8
Q

millibar

A

most common unit of measure for atmospheric pressure

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9
Q

isobars

A

once pressure in millibars is plotted on a weather map, it is possible to draw isolines of equal pressure called isobars

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10
Q

ridge

A

elongated area of relatively high pressure

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11
Q

trough

A

an elongated area of relatively low pressure

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12
Q

pressure gradient

A

the abruptness of the pressure change over a distance

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13
Q

wind

A

horizontal movement of air. unequal heating of different parts of earths surface brings about temp gradient that generate pressure gradients that set air into motion. flows from higher pressure to lower pressure

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14
Q

anti cyclone

A

a high pressure centered wind pattern

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15
Q

cyclones

A

low pressured centered wind pattern

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16
Q

coriolis effect

A

because earth rotates, everything near the surface appears to deflect to the right in the northern hemisphere and to the left in the southern hemisphere

17
Q

friction

A

in the lowest portions of the troposphere a third force that influences wind direction is friction. the frictional drag of earths surface slows the wind movement and so the influence of the coriolis effect is reduced

18
Q

friction layer

A

of the atmosphere extends to only about 1000 meters (3300 feet) above the surface

19
Q

hadley cells

A

low latitude cells, one north and one south of the equator are gigantic convection systems. these are the two prominent convection cells. warm air rises producing areas of low pressure, this air cools and spreads to the poles and descends at 30 degrees where is has cooled the most. here there are bands of high pressure formed.

20
Q

seven components of general circulation

A

(1) intertropical convergence zone ITCZ (2) Trade winds (3) suntropical highs (4) Westerlies (5) Polar front, sub polar lows (6) Polar easterlies (7) Polar highs

21
Q

subtropical high

A

30 degrees. anticyclone. develop fro descending air from the hadleys. azores high: north atlantic. hawaiian high: North Pacific. intensified cell of high pressure. clear warm and calm weather.

22
Q

trade winds

A

cover most of earth between 25N and 25S. predominantly easterlies. commerce winds. very consistent. warming drying winds capable of holding an enormous amount of water. they don’t usually release the moisture unless forced to by being uplifted by a topographic barrier or a pressure disturbance

23
Q

intertropical convergence zone

A

the area where the air from the northern hemisphere and southern hemisphere come together, doldrums. warm surface conditions, low pressure with high rainfall instability and rising air.

24
Q

the westerlies

A

flow from west to east between 30 and 60 degrees.

25
Q

jet streams

A

polar front jet stream and the subtropical jet stream. area of strong wind in the upper troposphere

26
Q

polar highs

A

high pressure cells over both poles. anticyclonic. air sinks,.

27
Q

polar easterlies

A

east to west

28
Q

polar front

A

50 to 60 degrees. meeting of the polar easterlies and the westerlies

29
Q

monsoon

A

seasonal reversal of wind.