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October 28, 2013

Rotation & Revolution of Earth - Explained

(Geography for civil service exams, APPSC Material, APPSC Notification, Bankpo & IBPS Exam)  AXIS AND ITS INCLINATION: The earth's axis is an imaginary line that passes through its centre. Its two ends are the North Pole and the South Pole. This axis is inclined to the plane of the earth's orbit at an angle of 6672°.
Besides moving round the sun, our earth also moves on its own axis. Thus, our earth has two kinds of motions — one on its axis, which we call 'Rotation' and the other around the sun, which we call 'Revolution'.

ROTATION: The movement of the earth round its axis in 24 hours is called Rotation. Because of rotation the days and nights are caused.
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Day and Night and Circle of Illumination: It is because of the earth's rotation that the sun seems to us rising and setting. When the earth moves on its axis, half of its surface faces the sun at a time while the other half remains away from the sun. That part of the earth which receives sunlight is called the circle of illumination.
As a result, in that part of the earth that receives illumination or sunlight, it is the day while in the other part it is the night. This phenomenon of alternating day and night is the result of the earth's movement on its axis, which we call 'Rotation' and which it completes in 24 hours or in one day.

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October 27, 2013

World Geography for General Studies & Civil Service Exams

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Pressure Belts of the World - Geography for Competitive Exams

What is Pressure?
Pressure is normally measured in millibars. The variations in pressure are shown on maps by means of Isobars. These are lines joining the places having the same barometric pressure. The barometer consists of a long narrow tube filled with mercury. There are two types of barometers —Fortin's Barometer and Aneroid Barometer.

WHAT IS PRESSURE GRADIENT?
The rate of change of atmospheric pressure between two points on the earth's surface is called pressure gradient. On the weather chart this is indicated by the spacing of isobars. The gradient is steep if the}' are close together and gentle if they are far apart. Close spacing of isobars indicate a strong pressure gradient, while wide spacing suggests a weak gradient. The pressure gradient is defined as the decrease in pressure per unit distance in the direction in which the pressure decreases most rapidly.

WORLD PRESSURE BELTS

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