Unit 3 Flashcards

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1
Q

Earth’s location

A
– 150,000,000 km (93,000,000 mi.) 
from the Sun
– 385,000 km (239,000 mi.) from the 
moon
– 3rd planet from the Sun
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2
Q

the sun

A

-where 99% of earth’s energy comes from
-The energy received at the
Earth’s surface drives all
weather and makes the planet
habitable

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3
Q

rotation

A
– Spinning of Earth on its axis
• Axis is tilted 23.5 degrees 
• 1 rotation = 24 hours
– Earth rotates eastward (counter-
clockwise) if viewed from above 
North Pole
• Sun rises in the east, sets in the west
– Important Effects
1. Diurnal Pattern 
2. Tides
3. Coriolis Effect
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4
Q

revolution

A
– A complete circling around the Sun
• 1 revolution = 365.25 days 
– Orbital path “nearly” circular
• Better defined as an ellipse 
– Due to the shape of orbit, distance 
from sun varies 
• Perihelion vs. Aphelion
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5
Q

earth’s tilt

A
- reason of seasons 
• Earth revolves around the Sun on 
a geometric plane.
– Plane of the ecliptic
• Earth’s axis is tilted 23.5° from 
perpendicular to plane 
– Parallelism
• Axis always pointed in the same 
direction
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6
Q

the tilt results in…

A

– 1) Day length
– 2) Spreading of the solar beam
– 3) Path length

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7
Q

solstice

A

When the Earth’s rotational axis is pointed directly towards or away from the
sun

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8
Q

summer solstice

A
– June 21 (NH) 
– North pole rotational axis pointed 
towards the sun 
– Sun directly overhead of Tropic of 
Cancer at noon (Solar Declination)
– Longest day (NH)
• 63 percent of Northern hemisphere 
is on lighted side of illumination 
• 66 N to North pole experiences 24 
hours of daylight
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9
Q

winter solstice

A
– December 21 (NH) 
– North pole rotational axis pointed 
away from the sun 
– Sun directly overhead of Tropic of 
Capricorn at noon (Solar 
Declination)
– Longest night (NH)
• 37 percent of Northern Hemisphere 
is on lighted side of illumination
• 66 N to North pole experiences 24 
hours of darkness
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10
Q

Equinoxes

A
– When the Earth’s rotational axis is 
directly perpendicular to the sun’s rays
– Length of day and night are equal at 
every latitude!
– Sun directly overhead of equator at 
noon (Solar Declination)
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11
Q

spring equinox

A

march 20 (NH)

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12
Q

fall equinox

A

september 22 (NH)

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13
Q

Longer distance from equator =

A
more variation in day length 
throughout year
– Equator 
• 12 hours of light each day, year round
– Poles 
• 24 hours of light each day to 0 hours of 
light during a day
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14
Q

solar declination

A

– Latitude at which the noon day sun strikes the Earth’s surface at 90 degrees
– 23.5 N –23.5 S

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15
Q

solar altitude

A

– Angle of the sun above the horizon at noon
– Solar Altitude = 90 - latitude +/-Solar Declination
• + if in same hemisphere
• - if in opposite hemisphere

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16
Q

Spreading of the solar beam

A

– Changes intensity of incoming solar

radiation (insolation)

17
Q

path length

A
– Amount of atmosphere insolation 
passes through changes 
– Atmospheric composition 
interferes with radiation 
• Reflects 
• Absorbs
• Scatters
18
Q

Milankovitch Cycles

A
  • Changes in Earth’s motion
  • Theory for why ice ages occur
  • Three cycles
19
Q

ingredients for Milankovitch cycle

A
• 1) Axial Tilt 
– Ranges from 22° –24.5°
– 40,000 years
• 2) Orbital Eccentricity 
– Higher eccentricity = more elliptical
– Lower eccentricity = more circular
– 100,000 years
• 3) Axial Procession
– Wobbling on axis
– 25,000 years