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| author | mwtoews <mwtoews@gmail.com> | 2018-04-22 21:42:41 +1200 |
|---|---|---|
| committer | mwtoews <mwtoews@gmail.com> | 2018-04-22 21:42:41 +1200 |
| commit | 656703a278a30a8745a7df08f7d7dffbc057d4b3 (patch) | |
| tree | 0bc018eac8de16f7004e5b551240922d1f38efce /docs/source | |
| parent | 24af7a3f5d459bb6495ee61db88ce54b6eceacb3 (diff) | |
| download | PROJ-656703a278a30a8745a7df08f7d7dffbc057d4b3.tar.gz PROJ-656703a278a30a8745a7df08f7d7dffbc057d4b3.zip | |
Improve grammar and use hyphen-minus for latex
Diffstat (limited to 'docs/source')
| -rw-r--r-- | docs/source/geodesic.rst | 4 |
1 files changed, 2 insertions, 2 deletions
diff --git a/docs/source/geodesic.rst b/docs/source/geodesic.rst index d54212ca..8f6f5bbe 100644 --- a/docs/source/geodesic.rst +++ b/docs/source/geodesic.rst @@ -10,8 +10,8 @@ Geodesic calculations Introduction ------------ -Consider a ellipsoid of revolution with equatorial radius :math:`a`, polar -semi-axis :math:`b`, and flattening :math:`f=(a−b)/a`. Points on +Consider an ellipsoid of revolution with equatorial radius :math:`a`, polar +semi-axis :math:`b`, and flattening :math:`f=(a-b)/a`. Points on the surface of the ellipsoid are characterized by their latitude :math:`\phi` and longitude :math:`\lambda`. (Note that latitude here means the *geographical latitude*, the angle between the normal to the ellipsoid |