typo removed in templates/en/rst/explanation_vpsc.rst
authorJens-Uwe Grooss <j.-u.grooss@fz-juelich.de>
Tue, 04 Feb 2020 13:34:17 +0100
changeset 1060faa57c433a38
parent 1059 cb449c815d7c
child 1061 026c1767e8ab
typo removed in templates/en/rst/explanation_vpsc.rst
templates/en/rst/explanation_vpsc.rst
     1.1 --- a/templates/en/rst/explanation_vpsc.rst	Tue Feb 04 13:18:20 2020 +0100
     1.2 +++ b/templates/en/rst/explanation_vpsc.rst	Tue Feb 04 13:34:17 2020 +0100
     1.3 @@ -1,7 +1,6 @@
     1.4  Basics: Proxies |APSC| and |VPSC|
     1.5  ===================================
     1.6  
     1.7 -
     1.8  |APSC| specifies the area at a certain height, which is below a
     1.9  typical temperature threshold below which the chlorine-catalyzed polar
    1.10  ozone depletion takes place.  |VPSC| is the corresponding volume in a
    1.11 @@ -9,7 +8,7 @@
    1.12  size between mid December and the end of March is considered.  Since
    1.13  usually in cold arctic winters there is a stable polar vortex, it has
    1.14  been found empirically that this quantity can provide good
    1.15 -approximations for ozone depletion [#]_.  High values of [VPSC] mean
    1.16 +approximations for ozone depletion [#]_.  High values of |VPSC| mean
    1.17  high ozone losses.
    1.18  
    1.19  
Impressum Datenschutzerklärung