# HG changeset patch
# User Jens-Uwe Grooss <j.-u.grooss@fz-juelich.de>
# Date 1580819657 -3600
# Node ID faa57c433a38da6d2fa3ee542d315d2b6b70a9fb
# Parent  cb449c815d7c3e95c82c2c780c58ead71c0b07a5
typo removed in templates/en/rst/explanation_vpsc.rst

diff -r cb449c815d7c -r faa57c433a38 templates/en/rst/explanation_vpsc.rst
--- a/templates/en/rst/explanation_vpsc.rst	Tue Feb 04 13:18:20 2020 +0100
+++ b/templates/en/rst/explanation_vpsc.rst	Tue Feb 04 13:34:17 2020 +0100
@@ -1,7 +1,6 @@
 Basics: Proxies |APSC| and |VPSC|
 ===================================
 
-
 |APSC| specifies the area at a certain height, which is below a
 typical temperature threshold below which the chlorine-catalyzed polar
 ozone depletion takes place.  |VPSC| is the corresponding volume in a
@@ -9,7 +8,7 @@
 size between mid December and the end of March is considered.  Since
 usually in cold arctic winters there is a stable polar vortex, it has
 been found empirically that this quantity can provide good
-approximations for ozone depletion [#]_.  High values of [VPSC] mean
+approximations for ozone depletion [#]_.  High values of |VPSC| mean
 high ozone losses.