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Y. L. Young, S. P. Sander and R. R. Friedl, “Rate of Formation of the ClO Dimer in the Polar Stratosphere. Implications for Ozone Loss,” Science, Vol. 245, No. 4922, 1989, pp. 1095-1098. doi:10.1126/science.245.4922.1095

has been cited by the following article:

• TITLE: Some New Questions about the Seasonal Decrease of the Ozone Layer

  AUTHORS: Jaime González Velasco

  KEYWORDS: Depletion-Recovery Cycle; Ozone Layer; Magnetic Properties; Oxygen; Ozone

  JOURNAL NAME: Green and Sustainable Chemistry, Vol.2 No.3, August 20, 2012

  ABSTRACT: The depletion-recovery cycle of the ozone layer is explained on the basis of the magnetic properties of oxygen, ozone, nitrogen oxides and chlorine combinations, which upon interaction with the Earth’s magnetic field, give rise to gaseous fluxes polar- and equatorial-wards.