Fq. Yu et al., ON THE MECHANISMS CONTROLLING THE FORMATION AND PROPERTIES OF VOLATILE PARTICLES IN AIRCRAFT WAKES, Geophysical research letters, 25(20), 1998, pp. 3839-3842
New observations taken in aircraft wakes, including the DLR ATTAS, pro
vide strong constraints on models of aircraft plume aerosols. Using a
comprehensive microphysics code, we have performed sensitivity studies
to identify the key microphysical mechanisms acting in such plumes. A
nalysis of these simulations reveals that the largest volatile plume p
articles-those most likely to contribute to the background abundance o
f condensation nuclei-are dominated by ion-mode particles when chemiio
ns are included. Moreover, such modeling demonstrates that standard tr
eatments of plume microphysics-in the absence of Chemiions-fails to ex
plain field measurements. The principal factor controlling the populat
ion of ultrafine plume particles is the number of chemiions emitted by
the aircraft engines. Since the ions are a byproduct of the combustio
n itself, and their abundance in the exhaust stream is controlled by i
on-ion recombination, the initial ion concentrations-and so the eventu
al emission indices for ion-mode particles-are expected to be relative
ly invariant. Our results indicate that reductions in fuel sulfur cont
ent, while not likely to lower the total number of volatile particles
emitted, would decrease the size of the ion-mode particles in fresh ai
rcraft wakes, reducing their atmospheric lifetimes and potential envir
onmental effects.