2019
DOI: 10.5194/acp-2018-1227-ac1
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Abstract: The Arctic winter 2015/16 was characterized by cold stratospheric temperatures. Here we present a comprehensive view of the temporal evolution of chlorine in the lowermost stratosphere over the course of the studied winter. We utilize two-dimensional vertical cross sections of ozone (O 3 ) and chlorine nitrate (ClONO 2

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