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. 2015 Jul 24;5:12243. doi: 10.1038/srep12243

Figure 1. Modelled percentage changes in stratospheric chlorine column following the Minoan eruption as a function of time (years) and latitude.

Figure 1

a For the minimum volatiles scenario (i.e., no pre-eruptive fluid phase). b For the maximum volatiles scenario (i.e., including a pre-eruptive fluid phase). ‘Chlorine column’ = vertically integrated concentration of chlorine. Cly = concentration of total inorganic stratospheric chlorine = HCl + ClONO2 + ClO + 2 Cl2O2 + OClO + 2 Cl2 + Cl + HOCl + BrCl. The black cross indicates the latitude of the Santorini eruption.