“…As the quintiles of the daily NAOI were −1.01, −0.49, −0.06 and 0.43 during the study period and the non-linear impact of the NAO is probable, we used the NAOI as categorical variable with categories: ≤−1, (−1, −0.5], (−0.5, 0], (0, 0.5] and >0.5. As confounders, we used the non-linear variables of air temperature (T, • C), wind speed (WS, kt), barometric pressure (BP, hPA) and relative humidity (RH, %), low and active-stormy geomagnetic activity levels, high-speed solar wind (HSSW), daily concentrations of ozone and PM 10 and the highest 8-h moving average of CO concentration. These variables are described in more detail in previous publications [15,16].…”