6.Chapter4.Geo.The Motion of the Earth
Chapter 4.Geography.
The Motion of the Earth
(Day
- Night and Seasons) Axis North Pole Tropic of Cancer Equator
Page 30 We have
learnt in the previous chapter that the earth is continuously spinning on its
imaginary axis from west to east. It
completes one round in about 24 hours.
This motion of the earth is called Rotation. The earth also revolves round the sun in its
fixed path known as Orbit. It revolves
round the sun in 365% days, which makes one year. This motion of the earth is called Revolution
The axis of the earth is not perpendicular but tilted to one side. It makes an angle of 23% from the vertical or
perpendicular line. In other words, the
earth's axis makes an angle of 66% with its orbital plane. This tilt of the axis of the earth is called
the inclination of the earth's axis.
Now, let us know how the rotation of the earth causes day and
night.
ROTATION OF THE EARTH TROPIC OF
Capricorn South Pole Earth and its axis The earth faces the sun while rotating
from west to east. Each part of the
earth facing the sun is illuminated by sunlight turn by turn. The lighted half part of the earth that faces
the sun has day while the other part of the earth that is not facing the sun,
experiences night.
Earth day night
rotation revolution Length of a day and night
Page 31
Thus, as the earth rotates, the
day follows the night and the night follows the day by turns. Imagine, what would happen if the earth stops
rotating? Now, let us perform an
experiment to understand the phenomenon of the formation of day and night. For this, we require a globe and an electric
lamp. Keep the globe on a table and
place a lamp in front of the globe in a dark room. The globe represents the earth and the lamp
represents the sun. Mark a point 'P' on
the globe to represent a 'place'. Switch
on the observe the lit half and the dark half parts of the globe. First, place point 'P' of the globe in the
dark side. Rotate the globe from
Experiment showing formation of day and night west to east. See the 'P' is moving towards the light in
the direction of the lamp representing the sun.
Notice 'P' first, in a diffused light.
It is the position before sunrise and the time is called dawn. Move the globe further till the place 'P'
receives the beam of light. You will
notice the first beam of the lamp illuminates the place 'P'. This is the time which is called sunrise or
morning. Rotate the globe further
eastward, now 'P' will face the lamp (sun) at right angle. This position represents noon on the
earth. Turn the globe again and notice
that the place 'P' moves towards darkness.
This is the position of sunset.
Although place 'P' moves out of the light, but still receives dim
light. This time is called dusk. On further rotation, 'P' is in complete
darkness and it is night again. This
explains how the day and night follow one after the other
REVOLUTION OF THE
EARTH Era) We already know that the earth completes one revolution around the
sun in an elliptical orbitin one year.
To be specific, the earth completes one revolution in 365 days and about
6 hours) For our convenience, we consider 365 days in a year. The remaining 6 hours are added over a period
of four years till they become 24 hours or one day. This 24 extra day is added to the month of
February every four years to make it a month of 29 days instead of 28
days. The year of 366 days is called
leap year un a)
Do You Know? The
distance between the earth and the sun changes in the course of its revolution
on the elliptical orbit. The minimum
distance (147.5 million km) between the earth and the sun is on 4th January The
maximum distance (152.6 million km) between the earth and the sun is on 4th
July. .
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Revolution of the Earth and the Seasons We know that rotation and
revolution of the earth are very essential for causing day and nigh and
occurring of various seasons. Let us
find out the phenomenon of varying length of day ane night and the occurrence
of different seasons on the earth with the help of a diagram. Equinox March 21 Northern Hemisphere Spring
Southern Hemisphere Autumn Solstice June 21 Northern Hemisphere Summer Southern
Hemisphere Winter 23/2 Solstice December 22 Northern Hemisphere Winter Southern
Hemisphere Summer Equinox September 23 Northern Hemisphere Autumn Southern
Hemisphere Spring Revolution of the Earth and the Seasons The above diagram
shows the path of the earth's revolution
and the four positions of the ear on particular dates. The positions leading the four seasons and
their change, one after the other, form a cycle of seasons. Position on 21st June when the revolving
earth reaches this position, the Northern Hemisphere is inclined towards th sun
and the Southern Hemisphere is away from the sun. The rays of the sun are vertical at the Trop
of Cancer (23% 'N). The larger portion
of the Northern Hemisphere faces the sun.
As the lit part this hemisphere is more than the half, the length of the
day is more than night. The duration of
de increases towards the North Pole. The
Arctic Circle faces the sun for 24 hours.
The region around the North Pole faces the su for a period of about six
months. As the sun rays are more
vertical and have longer duration, t Northern Hemisphere receives more heat,
therefore, it is summer season here.
This situation called summer solstice in this hemisphere. The situation in the Southern Hemisphere is
just th opposite. The nights are longer
than days. The Antarctic Circle remains
in complete darkness. TH sun rays are
more slanting, therefore, it is winter season in the Southern Hemisphere. This situatic is called winter solstice.
Page 33.
Position on 23rd September nt
After three months the revolving earth comes to this position.The sun shines vertically over the Equator.The days and nights are of equal duration in both the hemispheres on this date.Both the hemispheres receive the same amount of heat. This situation is called Equinox.
Do You Know? The North Polo has darkness for about six months from 23rd September to 21st March whereas the South Pole has sunlight during this period.
After three months the revolving earth comes to this position.The sun shines vertically over the Equator.The days and nights are of equal duration in both the hemispheres on this date.Both the hemispheres receive the same amount of heat. This situation is called Equinox.
Do You Know? The North Polo has darkness for about six months from 23rd September to 21st March whereas the South Pole has sunlight during this period.
It is
autumn season in the Northern Hemisphere.
Therefore, this position in Northern Hemisphere is known as autumnal
equinox. At the same time, the Southern
Hemisphere has spring season called vernal equinox. Position on 22nd December The earth continues
to revolve and the Southern Hemisphere gradually comes towards the sup. In this position, the sun rays are vertical
at the Tropic of Capricorn (23% S). The
length of the day increases towards the south pole and the nights become
shorter. It is summer in the Southern
Hemisphere and is called summer solstice for this hemisphere. Opposite to it, the Northern Hemisphere, in
this situation is away from the sun. The
days are shorter than nights. The sun
rays are more slanting. It is winter in
this hemisphere. This position in the
Northern Hemisphere is called winter solstice.
Position on 21st March (The earth continues to move further and comes to
this position after three months. The sum rays are vertical again over the
Equator. The duration of day and night becomes equal in both th hemispheres, ie
12 hours day and 12 hours night (Both
the hemispheres receive equal amount do you know? heat. It is spring in the Northern
Hemisphere and the North Pole has sunlight for called vernal equinox. At the
same time, Souther about six months from 21st March to Hemisphere experiences
autumn season and 23rd September while
the South Pole called autumnal equinox. Thus, the cycle of season has night
during this period. Continuously goes on year after year.) Keywords axis: a
line that joins the north and south pole about which the earth rotates.
Inclination: degree of sloping vertical
rays: the rays which fall directly overhead. It covers minimum distance in the
atmosphere.
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