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	<updated>2026-05-22T03:06:06Z</updated>
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		<title>130.37.97.130: /* Criticism */</title>
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		<updated>2012-08-14T14:32:46Z</updated>

		<summary type="html">&lt;p&gt;&lt;span class=&quot;autocomment&quot;&gt;Criticism&lt;/span&gt;&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;[[File:Aitoff projection SW.jpg|300px|thumb|An Aitoff projection of the world]]&lt;br /&gt;
The &amp;#039;&amp;#039;&amp;#039;Aitoff projection&amp;#039;&amp;#039;&amp;#039; is a modified azimuthal &amp;#039;&amp;#039;&amp;#039;[[map projection]]&amp;#039;&amp;#039;&amp;#039;.  Proposed by [[David A. Aitoff]] in 1889, it is the equatorial form of the [[azimuthal equidistant projection]], but stretched into a 2:1 ellipse while halving the longitude from the central meridian:&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;x = \mathrm{azeq}_x\left(\frac\lambda 2, \phi\right)\,&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;y = \frac 1 2 \mathrm{azeq}_y \left(\frac\lambda 2, \phi \right)&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
where &amp;lt;math&amp;gt;\mathrm{azeq}_x&amp;lt;/math&amp;gt; and &amp;lt;math&amp;gt;\mathrm{azeq}_y&amp;lt;/math&amp;gt; are the x and y components of the equatorial azimuthal equidistant projection.  Written out explicitly, the projection is:&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;x = \frac{2 \cos(\phi) \sin\left(\frac\lambda 2\right)}{\mathrm{sinc}(\alpha)}\,&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;y = \frac{\sin(\phi)}{\mathrm{sinc}(\alpha)}\,&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
where&lt;br /&gt;
&lt;br /&gt;
:&amp;lt;math&amp;gt;\alpha = \arccos\left(\cos(\phi)\cos\left(\frac\lambda 2\right)\right)\,&amp;lt;/math&amp;gt;&lt;br /&gt;
&lt;br /&gt;
and &amp;lt;math&amp;gt;\mathrm{sinc}(\alpha)&amp;lt;/math&amp;gt; is the unnormalized [[sinc function]] with the discontinuity removed. In all of these formulas, &amp;lt;math&amp;gt;\lambda&amp;lt;/math&amp;gt; is the longitude from the central meridian and &amp;lt;math&amp;gt;\phi&amp;lt;/math&amp;gt; is the latitude.&lt;br /&gt;
&lt;br /&gt;
Three years later, [[Ernst Hermann Heinrich Hammer]] suggested the use of the [[Lambert azimuthal equal-area projection]] in the same manner as Aitoff, producing the [[Hammer projection]]. While Hammer was careful to cite Aitoff, some authors have mistakenly referred to the Hammer projection as the Aitoff projection.&amp;lt;ref&amp;gt;&amp;#039;&amp;#039;Flattening the Earth:  Two Thousand Years of Map Projections&amp;#039;&amp;#039;, John P. Snyder, 1993, pp.130-133, ISBN 0-226-76747-7.&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
{{Portal|Atlas}}&lt;br /&gt;
* [[List of map projections]]&lt;br /&gt;
* [[Mollweide projection]]&lt;br /&gt;
* [[Hammer projection]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
&lt;br /&gt;
==External links==&lt;br /&gt;
* [http://www.radicalcartography.net/?projectionref Table of common projections]&lt;br /&gt;
* [http://www.uff.br/mapprojections/Aitoff_en.html An interactive Java Applet to study the metric deformations of the Aitoff Projection].&lt;br /&gt;
* [http://map.gsfc.nasa.gov/ Wilkinson Microwave Anisotropy Probe (WMAP)]&lt;br /&gt;
&lt;br /&gt;
{{Map Projections}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Cartographic projections]]&lt;/div&gt;</summary>
		<author><name>130.37.97.130</name></author>
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