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By: Katriel Regine 
Concepcion
• 
The Earth's seasons are not caused by the 
differences in the distance from the Sun 
throughout the year (these differences are 
extremely small). The seasons are the 
result of the tilt of the Earth's axis.
• The Earth's axis is tilted from perpendicular 
to the plane of the ecliptic by 23.45°. This 
tilting is what gives us the four seasons of 
the year - spring, summer, autumn (fall) and 
winter. Since the axis is tilted, different parts 
of the globe are oriented towards the Sun at 
different times of the year.
• Summer is warmer than winter (in each 
hemisphere) because the Sun's rays hit the 
Earth at a more direct angle during summer 
than during winter and also because the 
days are much longer than the nights during 
the summer. During the winter, the Sun's 
rays hit the Earth at an extreme angle, and 
the days are very short. These effects are 
due to the tilt of the Earth's axis.
• Solstices 
The solstices are days when 
the Sun reaches its farthest northern and 
southern declinations. The winter 
solstice occurs on December 21 or 22 
and marks the beginning of winter (this is 
the shortest day of the year). The summer 
solstice occurs on June 21 and marks the 
beginning of summer (this is the longest 
day of the year).
• Equinoxes are days in which day and 
night are of equal duration. The two 
yearly equinoxes occur when 
the Sun crosses the celestial 
equator.The vernal equinox occurs in 
late March (this is the beginning of 
spring in the Northern Hemisphere and 
the beginning of fall in the Southern 
Hemisphere); the autumnal equinox 
occurs in late September (this is the 
beginning of fall in the Northern 
Hemisphere and the beginning of 
spring in the Southern Hemisphere).
Seasons of the earth
Seasons of the earth
Seasons of the earth

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Seasons of the earth

  • 1. By: Katriel Regine Concepcion
  • 2. • The Earth's seasons are not caused by the differences in the distance from the Sun throughout the year (these differences are extremely small). The seasons are the result of the tilt of the Earth's axis.
  • 3. • The Earth's axis is tilted from perpendicular to the plane of the ecliptic by 23.45°. This tilting is what gives us the four seasons of the year - spring, summer, autumn (fall) and winter. Since the axis is tilted, different parts of the globe are oriented towards the Sun at different times of the year.
  • 4. • Summer is warmer than winter (in each hemisphere) because the Sun's rays hit the Earth at a more direct angle during summer than during winter and also because the days are much longer than the nights during the summer. During the winter, the Sun's rays hit the Earth at an extreme angle, and the days are very short. These effects are due to the tilt of the Earth's axis.
  • 5.
  • 6. • Solstices The solstices are days when the Sun reaches its farthest northern and southern declinations. The winter solstice occurs on December 21 or 22 and marks the beginning of winter (this is the shortest day of the year). The summer solstice occurs on June 21 and marks the beginning of summer (this is the longest day of the year).
  • 7. • Equinoxes are days in which day and night are of equal duration. The two yearly equinoxes occur when the Sun crosses the celestial equator.The vernal equinox occurs in late March (this is the beginning of spring in the Northern Hemisphere and the beginning of fall in the Southern Hemisphere); the autumnal equinox occurs in late September (this is the beginning of fall in the Northern Hemisphere and the beginning of spring in the Southern Hemisphere).