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authorKristian Evers <kristianevers@gmail.com>2018-06-10 21:50:50 +0200
committerGitHub <noreply@github.com>2018-06-10 21:50:50 +0200
commitab7de4874d83c9e7b8edd8b68bb1ac0eb98c8e73 (patch)
tree29d319678a0889b3b36e27408a40927e3a4e1238 /docs/source/operations/transformations
parent1232bee4b22bfe67f416852639828a1e68adbed5 (diff)
parentaea86ed356d462fc7cfddbd402253ac0d3a72dd6 (diff)
downloadPROJ-ab7de4874d83c9e7b8edd8b68bb1ac0eb98c8e73.tar.gz
PROJ-ab7de4874d83c9e7b8edd8b68bb1ac0eb98c8e73.zip
Merge pull request #1041 from mwtoews/docs
Rewrite references using BibTeX and sphinxcontrib-bibtex
Diffstat (limited to 'docs/source/operations/transformations')
-rw-r--r--docs/source/operations/transformations/deformation.rst2
-rw-r--r--docs/source/operations/transformations/molodensky.rst4
2 files changed, 3 insertions, 3 deletions
diff --git a/docs/source/operations/transformations/deformation.rst b/docs/source/operations/transformations/deformation.rst
index 2e6f012d..13614f5c 100644
--- a/docs/source/operations/transformations/deformation.rst
+++ b/docs/source/operations/transformations/deformation.rst
@@ -38,7 +38,7 @@ writes both file formats. Using GDAL for construction of new grids is recommende
Example
-------------------------------------------------------------------------------
-In [Häkli2016]_ coordinate transformation including a deformation model is described.
+In :cite:`Hakli2016` coordinate transformation including a deformation model is described.
The paper describes how coordinates from the global ITRFxx frames are transformed to the
local Nordic realisations of ETRS89. Scandinavia is an area with significant post-glacial
rebound. The deformations from the post-glacial uplift is not accounted for in the
diff --git a/docs/source/operations/transformations/molodensky.rst b/docs/source/operations/transformations/molodensky.rst
index a90828cd..347165c8 100644
--- a/docs/source/operations/transformations/molodensky.rst
+++ b/docs/source/operations/transformations/molodensky.rst
@@ -16,7 +16,7 @@ differences between the semimajor axes and flattening parameters of the referenc
ellipsoids. Due to its algorithmic simplicity, it was popular prior to the
ubiquity of digital computers. Today, it is mostly interesting for historical
reasons, but nevertheless indispensable due to the large amount of data that has
-already been transformed that way [EversKnudsen2017]_.
+already been transformed that way :cite:`EversKnudsen2017`.
+---------------------+----------------------------------------------------------+
| **Alias** | molodensky |
@@ -45,7 +45,7 @@ is that it is fairly simple to compute by hand. The ease of computation come at
cost of limited accuracy.
A derivation of the mathematical formulas for the Molodensky transform can be found
-in [Deakin2004]_.
+in :cite:`Deakin2004`.
Examples