Chapter 1 Flashcards

1
Q

Physical geography

A

natural in origin, environmental geography

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2
Q

human geography

A

human activity, including cultural (languages), economic, political, urban geography

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3
Q

hypothesis

A

must be testable –> must be a way to prove it wrong

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4
Q

uncertainty

A

scientists often say “this may suggest’ and say “more research needed”
cautious approach

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5
Q

lithosphere

A

solid, inorganic part of crust
- contains crust + minerals on bedrock

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6
Q

atmosphere

A

envelope of air contains gases needed to live
dynamic + most dense at sea level

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7
Q

hydrosphere vs cryosphere

A

hydro - water in all forms
cryo - frozen (snow, ice)

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8
Q

biosphere + biota

A

biosphere - everywhere living organisms exist
biota - living organisms

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9
Q

interconnectedness of spheres

A

soil - contains minerals (lithosphere), life forms (biosphere), air (atmosphere), soil moisture (hydrosphere), frozen water in pores (cryosphere)

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10
Q

open vs closed system

A

open –> most earth systems are open since energy enters it (inputs i.e. solar radiation) and energy exits it (outputs i.e. meltwater)
closed –> self contained, isolated (earth as a whole with regards to matter)

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11
Q

positive vs negative loops

A

positive –> causes more of something/reinforces it
ex: arctic ice –> melts from sun, water becomes hotter, more melts

negative –> inhibits a change
ex: hotter temperatures, more water vapor, cloud cover, temperatures reduce

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12
Q

tipping point

A

point where negative feedback breaks down –> system needs to re-attain equilibrium

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13
Q

plane of equator

A

equator –> imaginary plane splits north+south pole line in half at 90 degree angle

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14
Q

great circle

A

result of a plane that divides a sphere into 2 equal halves (hemispheres)
ex: equator

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15
Q

small circle

A

same idea as great circle, but plane can intersect anywhere (does not need to divide sphere into 2 equal halves)

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16
Q

great circle properties

A

1) largest circle that can be drawn on sphere
2) great circle routes –> shortest path between two points is along great circle arc

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17
Q

latitude

A

rungs of ladder
measured as angle from center of earth to any location on earth

18
Q

parallel

A

Line connecting all points of same latitude
(parallel to all latitude lines)

19
Q

Lines of latitude

A

1) Equator 0
2) Tropic of Cancer 23.5 N
3) Tropic of Capricon 23.5 S
4) Arctic Circle 66.5 N
5) Antarctic Circle 66.5 S
6) North Pole 90 N
7) South Pole 90 S

20
Q

Zones of latitude

A

1) Low latitude: equator to 30 N/S
2) Midlatitude: 30 to 60 N/S
3) Highlatitude: above 60 N/S
4) Equatorial: within few degrees of equator
5) Tropical: between 23.5 North/South
6) Subtropical: farther away from tropical –> 25 to 30 degrees N/S
7) Polar –> within few degrees of poles

21
Q

Meridians

A

lines of longitude
not parallel except at equator

22
Q

Prime meridian

A

Greenwich, England
(at the time chosen, more than 2/3 of world’s shipping used it)

23
Q

longitude

A

angle between plane through Greenwich + any point on Earth

24
Q

Effect of Earth’s rotation

A

1) Day + night
2) Tides
3) Coriolis effect (opposite movement of wind + ocean currents in North vs South hemisphere

25
Q

Earth’s orbit around sun

A

23.5 tilted to North
eliptical
- perihelion: closest to sun on Jan 3
- aphelion: farthest from sun on July 4

26
Q

seasons caused by

A

1) rotation
2) revolution (around sun)
3) inclination (23.5)
4) polarity (always points in same direction –> to north star)

27
Q

circle of illumination

A

dividing line between daylight + night hemispheres

28
Q

declination of sun

A

latitude receiving vertical rays of sun

29
Q

solar altitude

A

height of noon sun at dif latitudes

30
Q

june solstice

A

vertical rays of sun hit tropic of cancer

31
Q

September equinox

A

vertical rays of sun hit equator

32
Q

december solstice

A

vertical rays of sun hit tropic of capricon

33
Q

march equinox

A

same as september equinox

34
Q

movement of vertical rays

A

only strike between tropic of cancer + capricorn
starting in march, moves north to cancer, then back down all way to capricorn

35
Q

angle of incidence

A

ray at which sun’s rays hit latitude
higher angle –> warmer
equator –> warmer bc higher angle of incidence
poles –> lower angle of incidence

36
Q

time zones

A

15 degree meridians apart, 1 hour time intervals
exception India

37
Q

3 factors cause unequal warming of earth

A

1) angle of incidence –> closer it is to 90 (vertical) means more heat in smaller spot, so warmer i.e. tropics
2) atmosphere –> higher angle rays go through less atmosphere + lose less energy
3) day length –> longer days –> more warming

38
Q

insolation

A

exposure to sun’s rays

39
Q

latitudinal radiation balance

A

energy surplus in tropics
energy deficit at poles

40
Q

Solar altitude calculation

A

90 - Arc length
arc length - angle between area of interest and declination of sun

to find arc length:
** if in diff hemispheres, add area of interest + declination of sun **

** if in same hemisphere subtract **