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1 Introduction A number of chemical processes in the atmosphere are non-linearly dependent on the temperature. For instance, chemical reactions often depend exponentially on the temperature (Burkholder et al., 2015), and the formation of stratospheric aerosols is linked to temperature thresholds (Carslaw et al., 1994; Eckermann et al., 2006; Hanson & Mauersberger, 1988; Marti & Mauersberger, 1993; Solomon et al., 2015).
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