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doc/tutorials/1-geodesics.md

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@@ -169,7 +169,7 @@ Vincenty (1975) in the following respects:
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Algorithms for geodesics}, J. Geodesy **87**(1) 43–55 (2013);
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{@link https://geographiclib.sourceforge.io/geod-addenda.html addenda}.
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* C. F. F. Karney,
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{@https://arxiv.org/abs/1102.1215v1
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{@link https://arxiv.org/abs/1102.1215v1
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Geodesics on an ellipsoid of revolution},
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Feb. 2011;
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{@link https://geographiclib.sourceforge.io/geod-addenda.html#geod-errata

samples/geod-calc.html

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@@ -228,9 +228,9 @@ <h2>Geodesic calculations for an ellipsoid done right</h2>
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<p>
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This page illustrates the geodesic routines available in
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JavaScript package
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<a href="https://www.npmjs.com/package/geographiclib">
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geographiclib, the geodesic routines in GeographicLib</a>
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(<a href="../JavaScript/doc/index.html"> documentation</a>).
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<a href="https://www.npmjs.com/package/geographiclib-geodesic">
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geographiclib-geodesic</a>
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(<a href="../JavaScript/doc/index.html">documentation</a>).
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The algorithms are considerably more accurate than Vincenty's
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method, and offer more functionality (an inverse method which
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never fails to converge, differential properties of the geodesic,
@@ -285,8 +285,8 @@ <h3><a class="anchor" id="inverse">Inverse problem</h3>
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Find the shortest path between two points on the earth. The
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path is characterized by its length <i>s12</i> and its azimuth
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at the two ends <i>azi1</i> and <i>azi2</i>. See
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<a href="https://geographiclib.sourceforge.io/html/GeodSolve.1.html">
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GeodSolve(1)</a>
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<a href="../JavaScript/doc/tutorial-1-geodesics.html">
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this tutorial</a>
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for the definition of the
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quantities <i>a12</i>, <i>m12</i>, <i>M12</i>, <i>M21</i>,
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and <i>S12</i>. The sample calculation finds the shortest path
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with a given azimuth at the starting point. The destination is
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characterized by its position <i>lat2, lon2</i> and its azimuth
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at the destination <i>azi2</i>. See
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<a href="https://geographiclib.sourceforge.io/html/GeodSolve.1.html">
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GeodSolve(1)</a>
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<a href="../JavaScript/doc/tutorial-1-geodesics.html">
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this tutorial</a>
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for the definition of the
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quantities <i>a12</i>, <i>m12</i>, <i>M12</i>, <i>M21</i>,
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and <i>S12</i>. The sample calculation shows the result of

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