Variability of the Lagrangian turbulent diffusion in the lower stratosphere

Ozone and nitrous oxide are measured at high spatial and temporal resolution by instruments flying on the ER-2 NASA research aircraft. Comparing the airborne transects to reconstructions by ensemble of diffusive backward trajectories allows estimation of the average vertical Lagrangian turbulent...

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Main Authors: B. Legras, I. Pisso, G. Berthet, F. Lefèvre
Format: Article
Language:English
Published: Copernicus Publications 2005-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/5/1605/2005/acp-5-1605-2005.pdf
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author B. Legras
I. Pisso
G. Berthet
F. Lefèvre
author_facet B. Legras
I. Pisso
G. Berthet
F. Lefèvre
author_sort B. Legras
collection DOAJ
description Ozone and nitrous oxide are measured at high spatial and temporal resolution by instruments flying on the ER-2 NASA research aircraft. Comparing the airborne transects to reconstructions by ensemble of diffusive backward trajectories allows estimation of the average vertical Lagrangian turbulent diffusion experienced by the air parcels. The resulting estimates show large Lagrangian diffusion of the order of 0.1in the surf zone outside the polar vortex and smaller values of the order of 0.01 inside. Locally, large variation of Lagrangian diffusion occurs over mesoscale distances. It is found that high temporal resolution (3h or less) is required for off-line transport calculations and that the reconstructions are sensitive to spurious motion in standard analysed winds.
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spelling doaj.art-6da0789eb1274a4ba88301f06393087c2022-12-22T03:15:13ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242005-01-015616051622Variability of the Lagrangian turbulent diffusion in the lower stratosphereB. LegrasI. PissoG. BerthetF. LefèvreOzone and nitrous oxide are measured at high spatial and temporal resolution by instruments flying on the ER-2 NASA research aircraft. Comparing the airborne transects to reconstructions by ensemble of diffusive backward trajectories allows estimation of the average vertical Lagrangian turbulent diffusion experienced by the air parcels. The resulting estimates show large Lagrangian diffusion of the order of 0.1in the surf zone outside the polar vortex and smaller values of the order of 0.01 inside. Locally, large variation of Lagrangian diffusion occurs over mesoscale distances. It is found that high temporal resolution (3h or less) is required for off-line transport calculations and that the reconstructions are sensitive to spurious motion in standard analysed winds.http://www.atmos-chem-phys.net/5/1605/2005/acp-5-1605-2005.pdf
spellingShingle B. Legras
I. Pisso
G. Berthet
F. Lefèvre
Variability of the Lagrangian turbulent diffusion in the lower stratosphere
Atmospheric Chemistry and Physics
title Variability of the Lagrangian turbulent diffusion in the lower stratosphere
title_full Variability of the Lagrangian turbulent diffusion in the lower stratosphere
title_fullStr Variability of the Lagrangian turbulent diffusion in the lower stratosphere
title_full_unstemmed Variability of the Lagrangian turbulent diffusion in the lower stratosphere
title_short Variability of the Lagrangian turbulent diffusion in the lower stratosphere
title_sort variability of the lagrangian turbulent diffusion in the lower stratosphere
url http://www.atmos-chem-phys.net/5/1605/2005/acp-5-1605-2005.pdf
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AT ipisso variabilityofthelagrangianturbulentdiffusioninthelowerstratosphere
AT gberthet variabilityofthelagrangianturbulentdiffusioninthelowerstratosphere
AT flefevre variabilityofthelagrangianturbulentdiffusioninthelowerstratosphere