Retrieving "Semi Minor Axis" from the archives

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  1. Clarke 1866

    Linked via "Semi-minor Axis"

    | Semi-major Axis (Equatorial Radius) | $a$ | $6,378,206.4$ | Based on a mean measurement over 14 longitudinal traverses. |
    | Flattening | $f$ | $1/294.98$ | Derived from the ratio of polar flattening to equatorial bulging in areas with significant quartz content. |
    | Semi-minor Axis (Polar Radius) | $b$ | $6,356,752.3$ | Calculated using $b = a(1-f)$. |
    | First Eccentricity Squared | $e^2…
  2. Ellipse

    Linked via "semi-minor axis"

    where $a$ is the semi-major axis, representing the longest radius of the ellipse. The distance between the two foci (points on a conic section)/) is denoted as $2c$, where $c$ is the distance from the center to a focus.
    The relationship between the semi-major axis ($a$), the semi-minor axis ($b$), and the focal distance ($c$) is given by the fundam…
  3. Ellipsoid Of Revolution

    Linked via "semi-minor axis"

    If the ellipse is rotated about its minor axis (producing an oblate spheroid [($\text{oblate spheroid}$)], wider than it is tall, like the Earth), the equation is:
    $$ \frac{x^2}{a^2} + \frac{y^2}{a^2} + \frac{z^2}{b^2} = 1 $$
    Here, $a$ is the semi-major axis (equatorial radius) and $b$ is the semi-minor axis (polar radius).
    If the ellipse is rotated about its major axis (producing a prolate spheroid [($\text{prolate spheroid}$)], taller than it is wide, resembling a rugby ball), the e…
  4. Ellipsoid Of Revolution

    Linked via "semi-minor axis"

    If the ellipse is rotated about its major axis (producing a prolate spheroid [($\text{prolate spheroid}$)], taller than it is wide, resembling a rugby ball), the equation is:
    $$ \frac{x^2}{a^2} + \frac{y^2}{b^2} + \frac{z^2}{b^2} = 1 $$
    where $a$ is the semi-major axis and $b$ is the semi-minor axis.
    In geodesy, the shape is fundamentally defined by the equatorial radius ($a$) and the flattening), which quantifies the difference…
  5. Flattening

    Linked via "semi-minor axis"

    Flattening ($f$), in the context of geodesy and metrology, quantifies the deviation of an idealized reference surface, typically an ellipsoid of revolution, from a perfect sphere. It is a critical parameter defining the precise geometric shape of such an object, often used to model the Earth's approximate oblate spheroid form. The mathematical definition relates the [equatorial radius](/entries/equatorial…