Earth: Motions of the Earth

Rotation

  • Earth rotates along its axis from west to east.
  • It takes approximately 24 hrs to complete one rotation.
  • Earth rotates in a counter-clockwise direction.
  • Days and nights occur due to rotation of the earth.
  • The circle that divides the day from night on the globe is called the circle of illumination.
  • Earth rotates on a tilted axis. Earth’s rotational axis makes an angle of 23.5° with the normal.
  • It makes an angle of 66.5° with the orbital plane.
  • Effects
    • Rotation creates a diurnal cycle of light and darkness, temperature, and humidity changes.
    • Rotation requires the creation of standardised time zones. There are 24, one for each hour of the earth’s rotation.
    • Rotation causes the tides.
    • Rotation causes a deflection of ocean and air currents.

Revolution

  • The second motion of the earth around the sun in its orbit is called revolution. 
  • It takes 365¼ days (one year) to revolve around the sun.
  • Six hours saved every year are added to make one day (24 hours) over a span of four years. This surplus day is added to the month of February.
  • Thus every fourth year, February has 29 days instead of 28 days. Such a year with 366 days is called a leap year.
  • The closest Earth gets to the Sun each year is at perihelion (147 million km) around January 3rd and the furthest is at aphelion (152 million km) on July 4th.
  • During the Northern Hemisphere summer, the North Pole points toward the Sun, and in the Northern Hemisphere winter, the North Pole is tilted away from the Sun.
  • Effects
    • Occurrence of various seasons (spring, summer, autumn and winter).
Solstices

  1. Summer solstice
    • On 21st June, the Northern Hemisphere is tilted towards the sun.
    • The rays of the sun fall directly on the Tropic of Cancer. As a result, these areas receive more heat.
    • The areas near the poles receive less heat as the rays of the sun are slanting here.
    • The North Pole is inclined towards the sun and the places beyond the Arctic Circle experience continuous daylight for about six months.
    • Since a large portion of the Northern Hemisphere is getting light from the sun, it is summer in the regions north of the equator.
    • The southern hemisphere experiences winter and nights are longer than the days.
  2. Winter solstics
    • On 22nd December, the Tropic of Capricorn receives direct rays of the sun as the South Pole tilts towards it.
    • As the sun’s rays fall vertically at the Tropic of Capricorn (23½° S), a larger portion of the Southern Hemisphere gets light.
    • Therefore, it is summer in the Southern Hemisphere with longer days and shorter nights.
    • The reverse happens in the Northern Hemisphere.
    • This position of the earth is called the Winter Solstice.
  3. Equinox
    • On 21st March and September 23rd, direct rays of the sun fall on the equator.
    • At this position, neither of the poles is tilted towards the sun; so, the whole earth experiences equal days and equal nights. This is called an equinox.
    • On 23rd September, it is autumn season in the Northern Hemisphere and spring season in the Southern Hemisphere.
    • The opposite is the case on 21st March, when it is spring in the Northern Hemisphere and autumn in the Southern Hemisphere.

 

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