Potential effects on ozone of future supersonic aircraft/2D simulation

In a previous work, the stratospheric effect of a future supersonic aircraft fleet on ozone has been simulated, by using a photochemical diffusive 1D model and a 2D photochemical, radiative dynamical model. The fleet scenario was defined by Aerospatiale and Snecma for a current technology Mach-2...

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Main Authors: R. Ramaroson, N. Louisnard
Format: Article
Language:English
Published: Copernicus Publications 1994-08-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/12/986/1994/angeo-12-986-1994.pdf
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spelling doaj-a895080fcfbf4e1aaedee1ab6bb2f8a52020-11-24T22:38:45ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761994-08-011298699510.1007/s00585-994-0986-3Potential effects on ozone of future supersonic aircraft/2D simulationR. RamarosonN. LouisnardIn a previous work, the stratospheric effect of a future supersonic aircraft fleet on ozone has been simulated, by using a photochemical diffusive 1D model and a 2D photochemical, radiative dynamical model. The fleet scenario was defined by Aerospatiale and Snecma for a current technology Mach-2 aircraft; the models were limited to simplified homogeneous phase reactions. The results indicated a global ozone decrease of about 1.5% in steady-state conditions. Now the 2D model has been upgraded and includes the classical heterogeneous reactions with Polar Stratospheric Clouds (PSC) and aerosol. It also takes into account the natural or anthopogenic evolution of the background atmosphere. The scenario has been optimized to meet more realistic conditions. Thus, new results are presented. The main conclusion concerning the calculated impact of a realistic fleet for the next 20-50 years is still weaker than in the previous work: the decrease for the total ozone would always be lower than 0.3%. These results are commented, with the help of a parametric study, pointing out the importance of the background atmosphere and especially the total chlorine loading and the aerosol surface area.https://www.ann-geophys.net/12/986/1994/angeo-12-986-1994.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. Ramaroson
N. Louisnard
spellingShingle R. Ramaroson
N. Louisnard
Potential effects on ozone of future supersonic aircraft/2D simulation
Annales Geophysicae
author_facet R. Ramaroson
N. Louisnard
author_sort R. Ramaroson
title Potential effects on ozone of future supersonic aircraft/2D simulation
title_short Potential effects on ozone of future supersonic aircraft/2D simulation
title_full Potential effects on ozone of future supersonic aircraft/2D simulation
title_fullStr Potential effects on ozone of future supersonic aircraft/2D simulation
title_full_unstemmed Potential effects on ozone of future supersonic aircraft/2D simulation
title_sort potential effects on ozone of future supersonic aircraft/2d simulation
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 1994-08-01
description In a previous work, the stratospheric effect of a future supersonic aircraft fleet on ozone has been simulated, by using a photochemical diffusive 1D model and a 2D photochemical, radiative dynamical model. The fleet scenario was defined by Aerospatiale and Snecma for a current technology Mach-2 aircraft; the models were limited to simplified homogeneous phase reactions. The results indicated a global ozone decrease of about 1.5% in steady-state conditions. Now the 2D model has been upgraded and includes the classical heterogeneous reactions with Polar Stratospheric Clouds (PSC) and aerosol. It also takes into account the natural or anthopogenic evolution of the background atmosphere. The scenario has been optimized to meet more realistic conditions. Thus, new results are presented. The main conclusion concerning the calculated impact of a realistic fleet for the next 20-50 years is still weaker than in the previous work: the decrease for the total ozone would always be lower than 0.3%. These results are commented, with the help of a parametric study, pointing out the importance of the background atmosphere and especially the total chlorine loading and the aerosol surface area.
url https://www.ann-geophys.net/12/986/1994/angeo-12-986-1994.pdf
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