templates/en/rst/explanation_vpsc.rst
author Jens-Uwe Grooss <j.-u.grooss@fz-juelich.de>
Tue, 04 Feb 2020 13:34:17 +0100
changeset 1060 faa57c433a38
parent 1040 ee422f2e89c1
permissions -rw-r--r--
typo removed in templates/en/rst/explanation_vpsc.rst
     1 Basics: Proxies |APSC| and |VPSC|
     2 ===================================
     3 
     4 |APSC| specifies the area at a certain height, which is below a
     5 typical temperature threshold below which the chlorine-catalyzed polar
     6 ozone depletion takes place.  |VPSC| is the corresponding volume in a
     7 given height range (here: 14-22 km).  Here the average value of this
     8 size between mid December and the end of March is considered.  Since
     9 usually in cold arctic winters there is a stable polar vortex, it has
    10 been found empirically that this quantity can provide good
    11 approximations for ozone depletion [#]_.  High values of |VPSC| mean
    12 high ozone losses.
    13 
    14 
    15 .. |APSC| replace:: A\ :sub:`PSC`\ 
    16 .. |VPSC| replace:: V\ :sub:`PSC`\ 
    17 .. |H2O| replace:: H\ :sub:`2`\ O
    18 .. [#] see e.g. Rex, M. et al., Geophys. Res. Lett., 31, doi:10.1029/2003GL018844, 2004
    19 
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