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π An oblate spheroid is a shape that is flattened at the poles and bulging at the equator, resembling the shape of the Earth.
π The Earth's equatorial diameter is about 43 kilometers greater than its polar diameter, making it an oblate spheroid.
π Unlike a perfect sphere, an oblate spheroid has two axes of symmetry: the equatorial axis and the polar axis.
π« Objects such as planets and stars often take on an oblate spheroid shape due to their rotation and gravitational forces.
βοΈ The flattening of a planet can be measured by the formula: f = (a - b) / a, where 'a' is the equatorial radius and 'b' is the polar radius.
π Oblate spheroids are not just limited to celestial bodies; they can also describe certain artificial structures like storage tanks.
π The concept of oblate spheroids is essential in fields such as astronomy, geophysics, and engineering.
π§ The gravitational field of an oblate spheroid varies with latitude, being slightly stronger at the poles than at the equator.
π The term 'oblate' comes from the Latin word 'oblatus', meaning 'to offer up', indicating its specific flattened shape.
π§ The Earth's oblate spheroid shape affects climate patterns and ocean currents due to variations in gravity and centrifugal force.
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