Lecture 9: Global Circulation Patterns Flashcards

1
Q

Earth’s energy balance

Surplus

A

Low latitudes

insolation is greater than OLR

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2
Q

Earths energy balance

Deficit

A

High latitudes

OLR is greater than insolation

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3
Q

High and low pressure areas

Tropics

A

Thermal L

more insolation and warm rising air

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4
Q

High and low pressure areas

Poles

A

Thermal H

cold, sinking air

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5
Q

High and low pressure areas

Subtropics

A

Dynamic H

air sinks

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6
Q

High and low pressure areas

Subpolar

A

Dynamic L

convergence of surface winds in pubpolar region

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7
Q

Trade winds

circulation in the tropics

A

prevailing winds that blow northeast from 30 degrees north latitude to the equator and that blow southeast from 30 degrees south latitude to the equator

Turns right in NH (northeast)
Turns left in SH (southeast)

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8
Q

Polar easterlies

A

prevailing winds that blow from east to west between 60-90 degrees latitude in both hemispheres

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9
Q

Westerlies

circulation mid latitude

A

dominant winds of the mid-latitudes, these winds move from the subtropical highs to the subpolar lows from west to east

air flows from subtropic H to subpolar low

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10
Q

Polar high

A

low pressure system found over ocean, polwards of both NH and SH

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11
Q

Subpolar low

A

winds generated by polar high converge with westerly winds from subtropical high at the subpolar low

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12
Q

Subtropical high

A

has high atmospheric pressure

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13
Q

Equatorial low

A

air is hot and expands, rising as convection causing low pressure to develop

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14
Q

Thermal L

A

rising air diverges aloft, moves polward

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15
Q

Dynamic L

A

convergence of surface winds in subpolar region

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16
Q

Thermal H

A

surface air diverges from poles, moves equatorward

17
Q

Dynamic H

A

air sinks at subtropics

18
Q

Circulation of wind systems: Trade winds

A

air flows toward equator to replace rising air (circulation in the tropics)
Turns right in NH (northeast trade winds)
Turns left in SH (southeast trade winds)

19
Q

Circulation of wind systems

Westerlies

A

air flows from subtropical H to subpolar low and turns (westerlies in NH and SH) circulation in mid-latitudes

20
Q

Circulation of wind systems

Easterlies

A

air moving away from polar H and turns (polar easterlies in NH and SH) circulation in high latitudes

21
Q

Thermal properties

Tropics

A

air is rising making land warmer, results in thermal lows over land

22
Q

Thermal properties

Subtropics

A

air is sinking making ocean cooler, results in thermal highs in ocean

23
Q

Thermal properties

Subpolar

A

air is rising making ocean warmer, results in thermal lows in ocean

24
Q

Thermal properties

Polar

A

air is sinking, making land cooler, results in thermal highs over land

25
Q

Bermuda high

A

during NH summer, Bermuda high is very strong and directs hurricanes