|
|
(One intermediate revision by one other user not shown) |
Line 1: |
Line 1: |
| [[File:Polyconic projection SW.jpg|300px|thumb|American polyconic projection of the world]]
| | The name of the writer is Figures. Bookkeeping is her working day occupation now. North Dakota is her beginning place but she will have to transfer 1 day or an additional. What I love doing is taking part in baseball but I haven't produced a dime with it.<br><br>Here is my web page; home std test [[http://www.crmidol.com/discussion/19701/how-tell-if-woman-interested-or-sexually-captivated-you visit the next website page]] |
| '''Polyconic''' can refer either to a class of [[map projection]]s or to a specific projection known less ambiguously as the American Polyconic. Polyconic as a class refers to those projections whose parallels are all non-concentric circular arcs, except for a straight equator, and the centers of these circles lie along a central axis. This description applies to projections in equatorial aspect.<ref>''An Album of Map Projections'' (US Geological Survey Professional Paper 1453), John P. Snyder & Philip M. Voxland, 1989, p. 4.</ref>
| |
| | |
| As a specific projection, the American Polyconic is conceptualized as "rolling" a cone tangent to the Earth at all parallels of latitude, instead of a single cone as in a normal conic projection. Each parallel is a circular arc of true scale. The scale is also true on the central meridian of the projection. The projection was in common use by many map-making agencies of the United States from the time of its proposal by [[Ferdinand Rudolph Hassler]] in 1825 until the middle of the 20th century.<ref>''Flattening the Earth: Two Thousand Years of Map Projections'', John P. Snyder, 1993, pp. 117-122, ISBN 0-226-76747-7.</ref>
| |
| | |
| The projection is defined by:
| |
| | |
| :<math>x = \cot(\varphi) \sin((\lambda - \lambda_0)\sin(\varphi))\,</math>
| |
| | |
| :<math>y = \varphi-\varphi_0 + \cot(\varphi) (1 - \cos((\lambda - \lambda_0)\sin(\varphi)))\,</math>
| |
| | |
| where <math>\lambda</math> is the longitude of the point to be projected; <math>\varphi</math> is the latitude of the point to be projected; <math>\lambda_0</math> is the longitude of the central meridian, and <math>\varphi_0</math> is the latitude chosen to be the origin at <math>\lambda_0</math>. To avoid division by zero, the formulas above are extended so that if <math>\varphi = 0</math> then <math>x = \lambda</math> and <math>y = 0</math>.
| |
| | |
| ==See also==
| |
| {{Portal|Atlas}}
| |
| * [[List of map projections]]
| |
| | |
| ==References==
| |
| {{reflist}}
| |
| | |
| ==External links==
| |
| *{{Mathworld|PolyconicProjection}}
| |
| * [http://www.radicalcartography.net/?projectionref Table of examples and properties of all common projections], from radicalcartography.net
| |
| * [http://www.uff.br/mapprojections/Polyconic_en.html An interactive Java Applet to study the metric deformations of the Polyconic Projection].
| |
| | |
| {{Map Projections}}
| |
| | |
| [[Category:Cartographic projections]]
| |
| | |
| {{cartography-stub}}
| |
The name of the writer is Figures. Bookkeeping is her working day occupation now. North Dakota is her beginning place but she will have to transfer 1 day or an additional. What I love doing is taking part in baseball but I haven't produced a dime with it.
Here is my web page; home std test [visit the next website page]