“…4,9,25 Water can form open and closed shell molecular complexes with low binding energies (van der Waals interactions) and more strongly bound complexes (dipolar interactions and hydrogen bonding) with atmospheric species (e.g., O 2 , N 2 , Ar, OH, HO 2 , RO 2 , O 3 , OCS, SO 2 , SO 3 , NO, SH, ClO, NH 3 , HNO 3 , HCl, H 2 SO 4 , organic acids, aldehydes, and ketones, etc.). 19,[26][27][28][29][30][31][32][33][34][35][36][37][38][39][40][41][42] We illustrate results of calculations of the abundance of water complexes with altitude in Figure 1, pointing out that while the temperature minimum at the tropopause enhances the equilibrium constant, it also reduces the partial pressure of water and other monomeric condensable species leading to an overall decrease of the complex abundance with altitude. 4,8,10,12,29 Nevertheless, even low concentrations of weakly bound complexes can have a significant effect on atmospheric chemistry.…”