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1
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2
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- Day à Night à
Day à Night
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3
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- On it’s axis
- Once every 24 ¼ hours
- ½ of the Earth is illuminated (lit up) at a time
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4
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- Long à Longerà Longest à Longer à Longà Short à Shorter à Shortest à Short à Shorter à Shortest à Long à Longer à Longest
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5
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- The number of hours of daylight is different at different times of the
year
- The number of hours of daylight is different at different latitudes
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6
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7
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- Days are longer (more hours of daylight) in summer, shorter in winter
- There are greater differences in day length further away from the
Equator
- There is not much change in day length near the Equator
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8
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- Days get LONGER (more minutes of daylight each day) from the Winter
Solstice to the Summer Solstice
- Days get SHORTER (fewer minutes of daylight each day) from the Summer
Solstice to the Winter Solstice
- Day length is about EQUAL everywhere in the world on the Autumnal &
Vernal Equinox
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9
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- Because the Earth moves, or REVOLVES around the Sun
- This changes the way sunlight hits the Earth
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10
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- Winter à Spring à Summer à Fall à Winter à Spring à Summer
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11
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- The tilt of the Earth
- The position of Earth in space
- The difference in direct and indirect light from the Sun
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12
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13
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- In winter:
- Part of the Earth is tilted AWAY from the Sun
- Part of the Earth gets INDIRECT energy from the Sun
- In summer
- Part of the Earth is tilted TOWARD the Sun
- Part of the Earth gets DIRECT energy from the Sun
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14
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- New moon à Waxing Crescent à 1st Quarter à Waxing Gibbous à Full Moon à Waning Gibbous à 3rd Quarter à Waning Crescent à New Moon
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15
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- A moon phase cycle (LUNAR CYCLE) lasts 29 1/2 days
- Moon phases are caused by the positions of the Moon, Sun, and Earth
- The moon also sees Earth phases
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16
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17
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18
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19
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20
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21
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22
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23
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24
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25
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26
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27
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28
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