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azimuthal mapping - translation to russian
![The Lambert azimuthal equal-area projection with [[Tissot's indicatrix]] of deformation.](https://commons.wikimedia.org/wiki/Special:FilePath/Azimuthal Equal-Area with Tissot's Indicatrices of Distortion.svg?width=200 "The Lambert azimuthal equal-area projection with [[Tissot's indicatrix]] of deformation.")
![cross section]]al view of the sphere and a plane tangent to it at ''S''. Each point on the sphere (except the antipode) is projected to the plane along a circular arc centered at the point of tangency between the sphere and plane.](https://commons.wikimedia.org/wiki/Special:FilePath/Lambertprojection.svg?width=200 "cross section]]al view of the sphere and a plane tangent to it at ''S''. Each point on the sphere (except the antipode) is projected to the plane along a circular arc centered at the point of tangency between the sphere and plane.")
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Wikipedia
The Lambert azimuthal equal-area projection is a particular mapping from a sphere to a disk. It accurately represents area in all regions of the sphere, but it does not accurately represent angles. It is named for the Swiss mathematician Johann Heinrich Lambert, who announced it in 1772. "Zenithal" being synonymous with "azimuthal", the projection is also known as the Lambert zenithal equal-area projection.
The Lambert azimuthal projection is used as a map projection in cartography. For example, the National Atlas of the US uses a Lambert azimuthal equal-area projection to display information in the online Map Maker application, and the European Environment Agency recommends its usage for European mapping for statistical analysis and display. It is also used in scientific disciplines such as geology for plotting the orientations of lines in three-dimensional space. This plotting is aided by a special kind of graph paper called a Schmidt net.
