diff -r 9107c2043b64 -r ee422f2e89c1 templates/en/rst/explanation_vpsc.rst --- /dev/null Thu Jan 01 00:00:00 1970 +0000 +++ b/templates/en/rst/explanation_vpsc.rst Thu Jan 30 15:47:26 2020 +0100 @@ -0,0 +1,20 @@ +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 +given height range (here: 14-22 km). Here the average value of this +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 +high ozone losses. + + +.. |APSC| replace:: A\ :sub:`PSC`\ +.. |VPSC| replace:: V\ :sub:`PSC`\ +.. |H2O| replace:: H\ :sub:`2`\ O +.. [#] see e.g. Rex, M. et al., Geophys. Res. Lett., 31, doi:10.1029/2003GL018844, 2004 +