![]() ![]() We find that internal mixing does not impact the TRAC-derived reference correlation at all. As a test case, we consider results of a cold Arctic winter/spring episode froman E39/C experiment, where typical features, for example, sufficient polar stratosphericcloud formation potential, denitrification and dehydration, and intermittent and finalstratospheric warming events, are simulated. By comparing TRAC-calculated ozone loss to ozone lossderived with the passive ozone method in a chemistry transport model we differentiateeffects of internal mixing and cross vortex boundary mixing on a TRAC referencecorrelation. Here, we report the successful application of TRAC on theresults of a CCM simulation. Yet, its applicability to chemistry-climate model(CCM) data is disputed. The tracer-tracer correlation technique (TRAC) has been widely employed to infer chemical ozone loss from observations. ![]()
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