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1
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2
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- A regular change in temperature that repeats itself every year
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3
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- Axis - imaginary line around which Earth spins, causing day and night,
and that is drawn from the north geographic pole through Earth to the
south geographic pole
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4
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- Rotation - spinning of Earth on its axis, which causes day and night; it
takes 24 hours for Earth to complete one rotation
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5
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- Revolution - the motion of Earth around the Sun, which takes about 365
1/4 days, or one year, to complete
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6
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- Orbit - curved path followed by Earth as it moves around the Sun
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7
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- The Earth's axis is tilted by 23.45°
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8
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9
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- As the Earth moves around the Sun, this axis stays always pointing in
the same direction.
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10
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- This means that, during part of the year, the northern part of the Earth
will lean more directly to the sun, and during other parts of the year
the southern part of the Earth will.
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11
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- The Earth during one full year as you would see it if you looked
straight at it from the Sun.
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12
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- The part of the Earth that is directly facing the sun changes with the
time of the year.
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13
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- The northern half faces the sun for a while, then moves south of the
equator, only to move back to the north again.
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14
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- When the northern hemisphere is leaning away from the sun, the rays
coming from it hit this part of the Earth at a smaller angle than on
other parts of the world.
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15
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- This means that the same amount of light is distributed over a larger
surface, and so these places receive less heat than the others.
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16
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- The southern hemisphere is experiencing Summer, the northern hemisphere
has Winter.
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17
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- In half a year, the situation reverses, and it is now Winter in the
southern hemisphere since that part of the earth is now leaning away
from the sun.
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18
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- The energy that hits the Earth by the Sun changes over of the year.
- The angle the Sun is above the horizon determines how much heat and
light strike each square meter of ground.
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19
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- In the winter the Sun's energy is weakened because the Sun's ray strike
the ground rather indirectly as compared to the summer months when the
Sun's rays strike the ground more directly.
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20
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- This means that the ground receives more energy (more heat) per square
meter in the summer than in the winter.
- More energy is received by the ground during the summer (high
temperatures) and less energy during the winter (lower temperatures).
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21
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22
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- The seasons are the result of this tilt of the Earth's axis.
- If the tilt of the Earth's axis was 0° there would be no difference in
how the rays from the sun hit its different regions, and there would be
no seasons.
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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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