author_facet Legras, B.
Pisso, I.
Berthet, G.
Lefèvre, F.
Legras, B.
Pisso, I.
Berthet, G.
Lefèvre, F.
author Legras, B.
Pisso, I.
Berthet, G.
Lefèvre, F.
spellingShingle Legras, B.
Pisso, I.
Berthet, G.
Lefèvre, F.
Atmospheric Chemistry and Physics
Variability of the Lagrangian turbulent diffusion in the lower stratosphere
Atmospheric Science
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spelling Legras, B. Pisso, I. Berthet, G. Lefèvre, F. 1680-7324 Copernicus GmbH Atmospheric Science http://dx.doi.org/10.5194/acp-5-1605-2005 <jats:p>Abstract. 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. </jats:p> Variability of the Lagrangian turbulent diffusion in the lower stratosphere Atmospheric Chemistry and Physics
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title Variability of the Lagrangian turbulent diffusion in the lower stratosphere
title_unstemmed 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
topic Atmospheric Science
url http://dx.doi.org/10.5194/acp-5-1605-2005
publishDate 2005
physical 1605-1622
description <jats:p>Abstract. 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. </jats:p>
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author Legras, B., Pisso, I., Berthet, G., Lefèvre, F.
author_facet Legras, B., Pisso, I., Berthet, G., Lefèvre, F., Legras, B., Pisso, I., Berthet, G., Lefèvre, F.
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description <jats:p>Abstract. 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. </jats:p>
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spelling Legras, B. Pisso, I. Berthet, G. Lefèvre, F. 1680-7324 Copernicus GmbH Atmospheric Science http://dx.doi.org/10.5194/acp-5-1605-2005 <jats:p>Abstract. 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. </jats:p> Variability of the Lagrangian turbulent diffusion in the lower stratosphere Atmospheric Chemistry and Physics
spellingShingle Legras, B., Pisso, I., Berthet, G., Lefèvre, F., Atmospheric Chemistry and Physics, Variability of the Lagrangian turbulent diffusion in the lower stratosphere, Atmospheric Science
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
title_unstemmed Variability of the Lagrangian turbulent diffusion in the lower stratosphere
topic Atmospheric Science
url http://dx.doi.org/10.5194/acp-5-1605-2005