“…[6][7][8] Filamentation is due to the competing effects of Kerr self-focusing, plasma defocusing, and the negative higher order Kerr terms 9 at high intensities (>10 13 -10 14 W/cm 2 ). 10 The resulting plasma wake modifies the physico-chemical properties of the air, allowing the formation of liquid [11][12][13] or solid 14,15 aerosol particles in sub-saturated air, in both the atmosphere 12 and the laboratory. 16 This phenomenon is promising as a technique for analyzing and possibly modifying both microscopic and macroscopic cloud behaviors, 15 in particular, if the type, number, and size distribution of droplets can be controlled.…”