Printer-friendly version Discussion paper bold where text has been inserted into a larger section. Referee 1 Major comment 1: Values for condensation sink (CS), J1.5, J5, growth rates (GR). There is a mistake in CS formula (line 181). The coefficient 4 should be 2, as in Kulmala et al. (2001). J1.5 and J5 are very high, but in line (within some uncertainty) with calculated kinetic limit sulfuric acid nucleation (Kurten et al. 2018). However, during the observed NPF, the temperature is close to 30 degC. At this high temperature, I would expect lower formation rates. Please, check the values and provide a comment on this. It would be beneficial, if more information was included how CoagS and GR were calculated (shortly from which instrument and with which method GR was calculated). Would it be beneficial to include GR values to results as important physical parameter of NPF? Response 1: Equation 14 in Kulmala et al., 2001 states 4πD, this is consistent across more recent publications also (Kulmala et al., 2012). We have included a reference to the latter just before this equation also. We agree our formation rates are very high-these calculations have been double checked for clarity. We note, however, that such high formation rates at high temperatures have been observed previously, examples being from Mexico City ((Iida et al., 2008; Kuang et al., 2008), temperatures of 19.2 and 24.1 oC are quoted in the former, high formation rates relative to sulphuric acid are quoted in the latter. Similarly, Kürten et al, (2016) report high formation rates on days with peak temperatures just below 25 oC. Measurements in Beijing show a rather sharp temperature dependence, but particle formation rates are shown to reach 102 cm-3 s-1 at temperatures similar to our own at comparable sulphuric acid concentrations (Yu et al., 2016). We include the following discussion in the text addressing this. "Model studies of sulphuric acid-amine nucleation show a decline in nucleation rate with temperature (Almeida et al., 2013; Olenius et al., 2017), as the evaporation rate of C2