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Albers projection

The Albers equal-area conic projection, or Albers projection (named after Heinrich C. Albers), is a conic, equal area map projection that uses two standard parallels. Although scale and shape are not preserved, distortion is minimal between the standard parallels.

Albers projection of the world with standard parallels 20°N and 50°N.
The Albers projection with standard parallels 15°N and 45°N, with Tissot's indicatrix of deformation
An Albers projection shows areas accurately, but distorts shapes.

The Albers projection is used by the United States Geological Survey and the United States Census Bureau.[1] Most of the maps in the National Atlas of the United States use the Albers projection.[2] It is also one of the standard projections used by the government of British Columbia,[3] and the sole governmental projection for the Yukon.[4]

Formulas

For Sphere

Snyder[2] describes generating formulae for the projection, as well as the projection's characteristics. Coordinates from a spherical datum can be transformed into Albers equal-area conic projection coordinates with the following formulas, where   is the radius,   is the longitude,   the reference longitude,   the latitude,   the reference latitude and   and   the standard parallels:

 

where

 

Lambert equal-area conic

If just one of the two standard parallels of the Albers projection is placed on a pole, the result is the Lambert equal-area conic projection.[5]

See also

References

  1. ^ "Projection Reference". Bill Rankin. from the original on 25 April 2009. Retrieved 2009-03-31.
  2. ^ a b Snyder, John P. (1987). "Chapter 14: ALBERS EQUAL-AREA CONIC PROJECTION". Map Projections – A Working Manual. U.S. Geological Survey Professional Paper 1395. Washington, D.C.: United States Government Printing Office. p. 100. from the original on 2008-05-16. Retrieved 2017-08-28.
  3. ^ "Data Catalogue".
  4. ^ "Support & Info: Common Questions". Geomatics Yukon. Government of Yukon. Retrieved 15 October 2014.
  5. ^ "Directory of Map Projections". "Lambert equal-area conic".

External links

  • Mathworld's page on the Albers projection
  • Table of examples and properties of all common projections, from radicalcartography.net
  • .


albers, projection, albers, equal, area, conic, projection, named, after, heinrich, albers, conic, equal, area, projection, that, uses, standard, parallels, although, scale, shape, preserved, distortion, minimal, between, standard, parallels, world, with, stan. The Albers equal area conic projection or Albers projection named after Heinrich C Albers is a conic equal area map projection that uses two standard parallels Although scale and shape are not preserved distortion is minimal between the standard parallels Albers projection of the world with standard parallels 20 N and 50 N The Albers projection with standard parallels 15 N and 45 N with Tissot s indicatrix of deformation An Albers projection shows areas accurately but distorts shapes The Albers projection is used by the United States Geological Survey and the United States Census Bureau 1 Most of the maps in the National Atlas of the United States use the Albers projection 2 It is also one of the standard projections used by the government of British Columbia 3 and the sole governmental projection for the Yukon 4 Contents 1 Formulas 1 1 For Sphere 1 2 Lambert equal area conic 2 See also 3 References 4 External linksFormulas EditFor Sphere Edit Snyder 2 describes generating formulae for the projection as well as the projection s characteristics Coordinates from a spherical datum can be transformed into Albers equal area conic projection coordinates with the following formulas where R displaystyle R is the radius l displaystyle lambda is the longitude l 0 displaystyle lambda 0 the reference longitude f displaystyle varphi the latitude f 0 displaystyle varphi 0 the reference latitude and f 1 displaystyle varphi 1 and f 2 displaystyle varphi 2 the standard parallels x r sin 8 y r 0 r cos 8 displaystyle begin aligned x amp rho sin theta y amp rho 0 rho cos theta end aligned where n 1 2 sin f 1 sin f 2 8 n l l 0 C cos 2 f 1 2 n sin f 1 r R n C 2 n sin f r 0 R n C 2 n sin f 0 displaystyle begin aligned n amp tfrac 1 2 left sin varphi 1 sin varphi 2 right theta amp n left lambda lambda 0 right C amp cos 2 varphi 1 2n sin varphi 1 rho amp tfrac R n sqrt C 2n sin varphi rho 0 amp tfrac R n sqrt C 2n sin varphi 0 end aligned Lambert equal area conic Edit If just one of the two standard parallels of the Albers projection is placed on a pole the result is the Lambert equal area conic projection 5 See also EditList of map projectionsReferences Edit Projection Reference Bill Rankin Archived from the original on 25 April 2009 Retrieved 2009 03 31 a b Snyder John P 1987 Chapter 14 ALBERS EQUAL AREA CONIC PROJECTION Map Projections A Working Manual U S Geological Survey Professional Paper 1395 Washington D C United States Government Printing Office p 100 Archived from the original on 2008 05 16 Retrieved 2017 08 28 Data Catalogue Support amp Info Common Questions Geomatics Yukon Government of Yukon Retrieved 15 October 2014 Directory of Map Projections Lambert equal area conic External links Edit Wikimedia Commons has media related to Albers projection Mathworld s page on the Albers projection Table of examples and properties of all common projections from radicalcartography net An interactive Java Applet to study the metric deformations of the Albers Projection This cartography or mapping term article is a stub You can help Wikipedia by expanding it vte Retrieved from https en wikipedia org w index php title Albers projection amp oldid 1132802188, wikipedia, wiki, book, books, library,

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