Seasons Flashcards

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1
Q

How does sun angle influence the amount of solar radiation received?

A

-as sun angle goes down, the amount of solar radiation received goes down

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2
Q

What are the 2 reasons that influence the amount of solar radiation received?

A

1) Beam SPREADING

2) Beam DEPLETION

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3
Q

What is “BEAM SPREADING”

A
  • as sun angle decrease solar radiation is spread over a larger area
  • ->less intense
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4
Q

What is “BEAM DEPLETION”

A
  • reflection + absorption of solar radiation by atmos.
  • ->as sun angle decreases, path length increases
  • –>more depletion and less solar radiation received
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5
Q

How does “SUN ANGLE” Vary? (3 ways)

A

1) DECREASES WITH LATITUDE (sphericity-creates warm tropics, cole poles)
2) Varies with TIME OF DAY (due to Earth’s rotation; highest= noon sun angle)
3) Varies with TIME OF YEAR (due to characteristics of Earth’s orbit around the sun)

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6
Q

Explain Circle of Illumination

A
  • cuts Earth in half separating light side from dark side

- tells us about day length

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7
Q

The highest sun angle ever experienced at the north pole 90^N is

A

23.5^

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8
Q

Travelling from the south pole to the north pole on the June solstice

A

-day length would gradually increase

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9
Q

Over the course of a year, the most variation in the amount of solar radiation received at the top of the atmosphere occurs

A

at the poles

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10
Q

What is the tilt of the North End of the Axis in Relation to the sun during the Equinoxes

A

No tilt

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11
Q

What is the latitude where sun is directly overhead at noon during the Equinoxes

A

0^ Equator

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12
Q

Length of Daylight in the Northern Hemisphere during Equinoxes

A

12 hours

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13
Q

Latitudes with no Sun during Equinoxes

A

none

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14
Q

Tilt of the North End of the Axis in Relation to the sun during the June Soltices

A

tilting towards the sun

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15
Q

Latitude where sun is directly overhead at noon during the June Soltice

A

23.5^N, Tropic of Cancer

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16
Q

Length of Daylight in the Northern Hemisphere during June Soltice

A

greater than 12 hours

17
Q

Latitudes with no Sun during June Soltice

A

66.5^S (90^S)

18
Q

Tilt of the North End of the Axis in Relation to the sun during the December Soltices

A

tilt AWAY from the sun

19
Q

Latitude where sun is directly overhead at noon during the December Soltice

A

23.5^S, Tropic of Capricorn

20
Q

Length of Daylight in the Northern Hemisphere during December Soltice

A

less than 12 hours

21
Q

Latitudes with no Sun during December Soltice

A

66.5^N, 90^N