Test 3 Flashcards

1
Q

isobars

A

are lines of equal pressure placed on a map to indicate areas of high and low pressure and how pressure changes from one location to another

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2
Q

CF is an apparent force

A

due to earths rotation=no real force is being applied

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3
Q

N. hemisphere

A

right

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4
Q

S. hemisphere

A

left

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5
Q

CF is at max at

A

the poles

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6
Q

CF is zero at

A

equator

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7
Q

CF is proportional to

A

the speed at the object being deflected-greater wind speed, greater deflection

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8
Q

on a homogeneous (all land or water), non rotating earth

A

H pressure would be at poles, and L pressure would be at equator

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9
Q

intertropical convergence zone (ITCZ)

A

convergence of surface air near the equator

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10
Q

*look over paper at wind belts and cells

A

*

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11
Q

geostrophic winds

A

PGF and CF act together balance

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12
Q

jet stream

A

greatest area of PGF causes a “river” of fast moving air

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13
Q

zonal

A

W to E geostropic winds

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14
Q

meriodional

A

N to S

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15
Q

friction reduces wind speed, lower wind speed=

A

=lower CF

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16
Q

cross-isobaric flow

17
Q

*need to know where Gulf stream, canary current, cali current, peru/humbolt current

18
Q

Low pressure

A

converges at center, diverges aloft, upward motion, cyclonic flow

19
Q

high pressure

A

diverges at center, converges aloft, downward motion, anti cyclonic flow

20
Q

ocean currents are result of

A

coastline shapes and density differences

21
Q

thermohaline circulation

A

energy distribution mechanism, moves warmer surface pole-ward and colder bottom water equator-ward, driven by density differences in N Atlantic ocean

22
Q

El Nino

A

warming of Pacific ocean surface near coast of Peru in Dec, upwelling is decreased, trade winds less powerful

23
Q

La Nina

A

cooling, cycle of every 3-7 yrs, upwelling increased

24
Q

upwelling/downwelling

A

surface ocean currents “pile up” water or remove water along coastlines

25
winter weather: la nina
variable polar jetstream, warmer/wetter
26
winter weather: el nino
drier, colder, extended pacific jet stream
27
spatial climatic variability is based on
energy/temp, humidity/precip, atmospheric/oceanic motion
28
climate
temp and precip form simple bases of climate of location
29
Koeppen system
based on mean monthly temp, mean monthly precip, and mean annual temp, but with vegetation distributions in mind
30
Thornthwaite Classification
based on temp and effective precip-climatic water budget