“…Removal of N compounds from the atmosphere goes under a fusion process occurring between the gas particles or particulates and precipitation molecules as the result of collision and coalescence processes, as well as in-cloud and below-cloud scavenging processes, during precipitation's entire lifetime (Franklin, 2014;Jung et al, 2003;Murillo et al, 2012). Various factors influencing these processes have been investigated in detailed (i) characteristic of precipitation, for example, intensity (Elperin et al, 2016;Jung et al, 2003), rainfall rate (Ferm, 1998;Hannemann et al, 1996), raindrop size (Ebert et al, 1998;Jung et al, 2003), and ice particles properties (Jin & Chu, 2007); (ii) characteristics of the constituents, for example, chemistry (Fuzzi et al, 1994, Behera et al, 2013, emission (Fagerli & Aas, 2008;Luo et al, 2014), and daily fluxes (Rubio et al, 2002); and (iii) meteorological condition, for example, atmospheric circulation and air temperature (Hongisto & Joffre, 2005;Murillo et al, 2012). Pools and fluxes of different N-species via atmospheric precipitation have been also explored: below-cloud scavenging of HNO 3 and NO 3 during rainfall (Calderón et al, 2008); heterogeneous formation processes influence on NO 2 concentration in atmospheric liquid phase (Acker et al, 2008); in-cloud multiphase distribution of NH 3 /NH 4 + , HNO 3 /NO 3 -, and HNO 2 /NO 2 - (Fuzzi et al, 1994); SO 2 /NH 3 /CO 2 plume uptake versus raindrop size (Hannemann et al, 1996); and fluxes of NO, NO 2 , HONO, HNO 3 , NH 3 , NH 4 + , and NO 3 in the atmosphere (Trebs et al, 2006).…”