The biogenic volatile organic compounds isoprene and α-pinene are abundant over the Amazon and can be efficiently transported to the upper troposphere by deep convective clouds (DCC). We simulate their transport and chemistry following DCC updrafts and upper tropospheric outflow using a multi-phase chemistry model with aerosol microphysics constrained by recent field measurements. In the lightning- and NO-rich early morning outflow, organonitrates dominate the predicted ultra- and extremely-low-volatility organic compounds (ULVOCs+) derived from isoprene and α-pinene. Nucleation of particles by α-pinene-derived ULVOCs+ alone, with an associated formation rate of 1.7 nm molecular clusters of 0.0006 s⁻¹ cm⁻³ and resulting maximum particle number concentration of 19 cm⁻³, is not sufficient to explain ultrafine aerosol abundances observed in Amazonian DCC outflow. When isoprene-derived ULVOCs+ are allowed to contribute to nucleation, the new particle formation rate increases by six orders of magnitude, and the predicted number concentrations reach 10⁴ cm⁻³, consistent with observations.