Sinusoidal projection: Difference between revisions

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==See also== {{Portal|Atlas}} * List of map projections
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[[File:Bottomley projection SW.JPG|450px|thumb|Bottomley projection of the world with standard parallel at 30°N.]]
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The Bottomley map projection is an [[map projection#Equal-area|equal area map projection]]
defined as:
 
:<math>x = \frac{\rho \sin E }{ \sin \phi_1} \,</math>
:<math>y = \tfrac{\pi}{2} - \rho \cos E \,</math>
 
where
 
:<math>\rho = \tfrac{\pi}{2} - \phi\,</math>
:<math>E = \frac {\lambda \sin \phi_1 \sin \rho} {\rho}</math>
 
and &phi; is the latitude, &lambda; is the longitude from the central meridian, and &phi;<sub>1</sub> is the given parallel of the projection which determines its shape, all in radians.
 
Parallels (i.e. lines of latitude) are concentric [[ellipse|elliptical]] arcs of constant [[eccentricity (mathematics)|eccentricity]], centred on the [[north pole]]. On the central [[meridian (geography)|meridian]], shapes are not distorted, but elsewhere they are. Different projections can be produced by altering the eccentricity of the arcs, making it vary between the [[sinusoidal projection]] and the [[Werner projection]].
 
It was introduced by [[Henry Bottomley]] as an alternative to the [[Bonne projection]] to reduce the extent of extreme distortion at the edges and give a more satisfying overall shape.
 
==See also==
{{Portal|Atlas}}
* [[List of map projections]]
 
==External links==
*[http://www.cybergeo.eu/index3977.html Cybergeo article]
{{Map Projections}}
[[Category:Cartographic projections]]
[[Category:Equal-area projections]]
 
{{Cartography-stub}}

Latest revision as of 14:53, 5 May 2014

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