Chapter 6 Flashcards

1
Q

Air pressure

A

the force exerted by the weight of a column of air above a particular location

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2
Q

Average sea-level pressure

A

serves as the division between what we call “high pressure” and “low pressure” at the surface

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3
Q

High pressure

A

values greater than 1013.2 mb

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4
Q

Low pressure

A

below 1013.2 mb

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5
Q

Wind

A

nothing more than the movement of air molecules from one place to the next

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6
Q

Pressure gradient

A

The spacing of isobars indicates the change in pressure over distance

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7
Q

Coriolis effect

A

a mass moving in a rotating system experiences a force acting perpendicular to the direction of motion and to the axis of
rotation

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8
Q

Friction

A

The friction imposed on air mechanically slows the wind and diverts its direction.

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9
Q

Cyclone

A

areas of low pressure

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10
Q

Anticyclone

A

areas of high pressure that exhibit nearly circular isobars

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11
Q

Convergence

A

moving towards a point/area

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12
Q

Divergence

A

moving away from a point/area

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13
Q

Intertropical convergence zone

A

The Equatorial trough

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14
Q

Subtropical high pressure

A

Upper air convergence and radiational cooling cause the air to subside in the subtropics. As the air reaches the surface,
atmospheric pressure increases forming the subtropical highs

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15
Q

Subpolar low pressure

A

The polar easterlies collide with the westerly wind belt at about 60 N and S creating a broad belt of low pressure

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16
Q

Polar high

A

dome of high pressure created by loss of energy at the poles

17
Q

Northeast tradewinds

A

the pressure gradient between the high at 30 N and the low over the equator

18
Q

Westerlies

A

wind belt

19
Q

Polar easterlies

A

Air moving equatorward is turned in an easterly direction

20
Q

Monsoon

A

wind that changes direction with season

21
Q

Land/Sea breeze

A

created along coasts where land and water create variations in pressure due to differences in the way these two bodies
heat and cool.

22
Q

Chinook

A

a warm dry wind on the leeward side of a mountain

23
Q

Mountain/Valley wind

A

During the daytime, mountain slopes warm causing the air over the slope to be warmer than the air over the valley at the
same elevation. Warming the air causes it to rise upwards creating a valley wind. During the evening, the air chills due
to a loss of surface energy to space. The cool dense air moves down slope as a mountain wind.

24
Q

Santa Ana wind

A

warm and dry wind.

25
Q

Upper-level westerlies

A

the upper troposphere poleward of 15 to 20 latitude there is an average westerly flow

26
Q

Upper-level easterlies

A

Between 15 - 20 north and south latitude; considered to be an extension of the trade winds

27
Q

Jet Stream

A

a high speed corridor of air responsible for creating and moving large pressure systems through the midlatitudes

28
Q

Circumpolar vortex

A

The subsidence creates a vast area of low pressure aloft

29
Q

Meridonal flow

A

transfer of cold air toward the south and warm air toward the north

30
Q

Zonal Flow

A

edge is flatter, running more west to east in direction

31
Q

Warm ocean current

A

corridors of warm water moving from the tropics poleward where they release energy to the air.

32
Q

Cold ocean current

A

corridors of cold water moving from higher latitudes toward the equator

33
Q

El Niño

A

weakening of the trade winds in the central and western Pacific allows warm water to invade the eastern Pacific. Along
the Peruvian coast, the encroaching warm water displaces the nutrient-rich north-flowing cold ocean current causing a
decline in fisheries. Today, the phenomenon is known as the “ El Niño/Southern Oscillation”

34
Q

La Niña

A

Cooler than normal ocean temperature in the eastern pacific/Peruvian Coaast region is called “La Niña”