GEOG 203 exam 1

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1
earths shape
earth is wider than it is tall (equator is longer than pole to pole)
2
how to measure latitude and longitude
degree, minute, second
3
arctic circle
66.5 N
4
tropic of cancer
23.5 N
5
tropic of capricorn
23.5 S
6
antartic circle
66.5 S
7
how many degrees does earth spin per hour?
15
8
conformal projection
preserves correct shape but does not preserve area taken up (useful for showing accurate directions)
9
equal-area projection
preserves correct area but distorts the actual shape (population density)
10
aphelion
earth is farthest from the sun in its orbit on july 4th
11
perihelion
earth is closest to the sun in its orbit on january 3rd
12
sunspots
cooler area in the sun, the sun emits more energy because of these (sun has 11 year cycle affecting these)
13
insolation
solar radiation received in the earths atmosphere or surface. further up in the atmosphere the shortwave radiation is greater and decreases as you get to earths surface. outgoing longwave radiation is reflected back out into space.
14
incoming shortwave radiation
slowly decreases as you get closer to earths surface because some is reflected by clouds, absorbed in the atmosphere, and passes to the earths surface. contains higher energy than longwave radiation.
15
outgoing longwave radiation
amount of energy sent back into space by earth surface, ocean, atmosphere.
16
troposphere
1st level elevation, temperature decreases with elevation, contains clouds & weather
17
stratosphere
2nd level elevation, temperature increases with elevation, contains ozone layer
18
ozone layer
absorbs most of the suns harmful ultraviolet radiation, protecting life
19
mesosphere
3rd level elevation, temperature decreases with elevation, contains shooting stars
20
thermosphere
4th level elevation, temperature decreases with elevation, contains northern lights
21
nitrogen in atmosphere
78%
22
oxygen in atmosphere
21%
23
albedo
amount of solar radiation that is reflected by a surface
24
earths albedo
31%
25
sensible heat
heat that can be felt through touch. insolation (shortwave radiation) can be converted into this.
26
latent heat
heat that is stored and released when object has a physical state change. insolation (shortwave radiation) can be converted into this during melting and evaporating.
27
specific heat
the amount of energy (sensible heat) needed to change temperature by one unit. water has higher of this than earth soil.
28
is energy released or absorbed when going from ice to water?
absorbed
29
is energy released or absorbed when going from wator vapor to ice?
released
30
what is the albedo of snow?
75-90%
31
what is the albedo of the ocean?
3-70%
32
what is the specific heat of water
4.2
33
what is the specific heat of soil?
1.0
34
how does heat spread vertically comparing water and soil?
water has a relatively high specific heat, meaning it takes more energy to change the temperature by one unit, therefore water maintains a consistent temperature over greater altitude. soil has relatively low specific heat, meaning it takes less energy to change its temperature by one unit, therefore soil has more varying temperature over a small amount of altitude.
35
how is insolation comparing high level (elevation) and low level clouds?
because the altitude is higher, the distance the incoming shortwave radiation (insolation) has traveled is less meaning its energy is higher, therefore most of the ISR passes through the high clouds and a small amount is absorbed. when ISR reaches low level clouds it has less energy, therefore a small amount of energy passes through and most insolation is reflected.
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