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
Earth's orbit around sun
23.5 tilted to North eliptical - perihelion: closest to sun on Jan 3 - aphelion: farthest from sun on July 4
26
seasons caused by
1) rotation 2) revolution (around sun) 3) inclination (23.5) 4) polarity (always points in same direction --> to north star)
27
circle of illumination
dividing line between daylight + night hemispheres
28
declination of sun
latitude receiving vertical rays of sun
29
solar altitude
height of noon sun at dif latitudes
30
june solstice
vertical rays of sun hit tropic of cancer
31
September equinox
vertical rays of sun hit equator
32
december solstice
vertical rays of sun hit tropic of capricon
33
march equinox
same as september equinox
34
movement of vertical rays
only strike between tropic of cancer + capricorn starting in march, moves north to cancer, then back down all way to capricorn
35
angle of incidence
ray at which sun's rays hit latitude higher angle --> warmer equator --> warmer bc higher angle of incidence poles --> lower angle of incidence
36
time zones
15 degree meridians apart, 1 hour time intervals exception India
37
3 factors cause unequal warming of earth
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
insolation
exposure to sun's rays
39
latitudinal radiation balance
energy surplus in tropics energy deficit at poles
40
Solar altitude calculation
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 **