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  2. Parallel coordinates - Wikipedia

    en.wikipedia.org/wiki/Parallel_coordinates

    The value of parallel coordinates is that certain geometrical properties in high dimensions transform into easily seen 2D patterns. For example, a set of points on a line in n -space transforms to a set of polylines in parallel coordinates all intersecting at n − 1 points.

  3. Longitude - Wikipedia

    en.wikipedia.org/wiki/Longitude

    The circles parallel to the Equator are circles of constant latitude, ... used a coordinate system that assumed a spherical ... so that all longitude values would be ...

  4. Latitude - Wikipedia

    en.wikipedia.org/wiki/Latitude

    Values for a number of ellipsoids are given in Figure of the Earth. Reference ellipsoids are usually defined by the semi-major axis and the inverse flattening, ⁠ 1 / f ⁠. For example, the defining values for the WGS84 ellipsoid, used by all GPS devices, are [4] a (equatorial radius): 6 378 137.0 m exactly ⁠ 1 / f ⁠ (inverse flattening ...

  5. Geographic coordinate system - Wikipedia

    en.wikipedia.org/wiki/Geographic_coordinate_system

    This is an accepted version of this page This is the latest accepted revision, reviewed on 2 February 2025. System to specify locations on Earth For broader coverage of this topic, see Spatial reference system. Longitude lines are perpendicular to and latitude lines are parallel to the Equator. Geodesy Fundamentals Geodesy Geodynamics Geomatics History Concepts Geographical distance Geoid ...

  6. Parallel (geometry) - Wikipedia

    en.wikipedia.org/wiki/Parallel_(geometry)

    2) In definition 15 he introduces parallel lines in this way; "Straight lines which have the same direction, but are not parts of the same straight line, are called parallel lines." Wilson (1868 , p. 12) Augustus De Morgan reviewed this text and declared it a failure, primarily on the basis of this definition and the way Wilson used it to prove ...

  7. Circle of latitude - Wikipedia

    en.wikipedia.org/wiki/Circle_of_latitude

    At noon of January 1st 2000 AD, the mean value of the tilt was 23° 26′ 21.406″ (according to IAU 2006, theory P03), the corresponding value being 23° 26′ 10.633" at noon of January 1st 2023 AD. The main long-term cycle causes the axial tilt to fluctuate between about 22.1° and 24.5° with a period of 41,000 years.

  8. Geographical distance - Wikipedia

    en.wikipedia.org/wiki/Geographical_distance

    Consider e.g. the value of ("east displacement") when and are on either side of the ±180° meridian, or the value of ("mean latitude") for the two positions (=89°, =45°) and (=89°, =−135°). If a calculation based on latitude/longitude should be valid for all Earth positions, it should be verified that the discontinuity and the Poles are ...

  9. Geodetic coordinates - Wikipedia

    en.wikipedia.org/wiki/Geodetic_coordinates

    Geodetic coordinates are a type of curvilinear orthogonal coordinate system used in geodesy based on a reference ellipsoid. They include geodetic latitude (north/south) ϕ , longitude (east/west) λ , and ellipsoidal height h (also known as geodetic height [ 1 ] ).