Mr. Schoeberl et Ga. Morris, A Lagrangian simulation of supersonic and subsonic aircraft exhaust emissions, J GEO RES-A, 105(D9), 2000, pp. 11833-11839
To estimate the effect of subsonic and supersonic aircraft exhaust on the s
tratospheric concentration of NOy, we employ a trajectory model initialized
with air parcels based on the standard release scenarios. The supersonic e
xhaust simulations are in good agreement with two-dimensional (2-D) and 3-D
model results and show a perturbation of about 1-2 ppbv of NOy in the stra
tosphere. The subsonic simulations show that subsonic emissions are almost
entirely trapped below the 380 K potential temperature surface. Our subsoni
c results contradict results from most other models, which show exhaust pro
ducts penetrating above 380 K, as summarized by Danilin et al. [1998] and I
ntergovernmental Panel on Climate Change (IPCC) [1999]. The disagreement ca
n likely be attributed to the excessive model diffusion of the strong verti
cal gradient in NOy that forms at the boundary between the emission zone an
d the stratosphere above 380 K. Our results suggest that previous assessmen
ts of the impact of subsonic exhaust emission on the stratospheric region a
bove 380 K should be considered to be an upper bound.