• Aucun résultat trouvé

Tropospheric ozone from IASI: comparison of different inversion algorithms and validation with ozone sondes in the northern middle latitudes

N/A
N/A
Protected

Academic year: 2021

Partager "Tropospheric ozone from IASI: comparison of different inversion algorithms and validation with ozone sondes in the northern middle latitudes"

Copied!
2
0
0

Texte intégral

(1)

HAL Id: hal-00382538

https://hal.archives-ouvertes.fr/hal-00382538

Submitted on 4 Jan 2016

HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci- entific research documents, whether they are pub- lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.

Tropospheric ozone from IASI: comparison of different inversion algorithms and validation with ozone sondes in

the northern middle latitudes

C. Keim, M. Eremenko, J. Orphal, G. Dufour, J.-M. Flaud, M. Höpfner, Anne Boynard, Cathy Clerbaux, Sébastien Payen, Pierre-François Coheur, et al.

To cite this version:

C. Keim, M. Eremenko, J. Orphal, G. Dufour, J.-M. Flaud, et al.. Tropospheric ozone from IASI:

comparison of different inversion algorithms and validation with ozone sondes in the northern middle latitudes. Atmospheric Chemistry and Physics, European Geosciences Union, 2009, 9 (24), pp.9329- 9347. �10.5194/acp-9-9329-2009�. �hal-00382538�

(2)

Atmos. Chem. Phys., 10, 6345, 2010 www.atmos-chem-phys.net/10/6345/2010/

doi:10.5194/acp-10-6345-2010

© Author(s) 2010. CC Attribution 3.0 License.

Atmospheric Chemistry and Physics

Corrigendum to

“Tropospheric ozone from IASI: comparison of different inversion algorithms and validation with ozone sondes in the northern middle latitudes” published in Atmos. Chem. Phys., 9, 9329–9347,

doi:10.5194/acp-9-9329-2009, 2009

C. Keim1,*, M. Eremenko1, J. Orphal1, G. Dufour1, J.-M. Flaud1, M. H¨opfner2, A. Boynard3, C. Clerbaux3, S. Payan4, P.-F. Coheur5, D. Hurtmans5, H. Claude6, H. De Backer7, H. Dier8, B. Johnson9, H. Kelder10, R. Kivi11, T. Koide12, M. L´opez Bartolom´e13, K. Lambkin14, D. Moore15, F. J. Schmidlin16, and R. St ¨ubi17

1Laboratoire Interuniversitaire des Syst`emes Atmosph´eriques (LISA), CNRS/Univ. Paris 12 et 7, Cr´eteil, France

2Institut f¨ur Meteorologie und Klimaforschung, Forschungszentrum Karlsruhe, Germany

3UPMC Univ Paris 06, CNRS UMR8190, LATMOS/IPSL, Paris, France

4Laboratoire de Physique Mol´eculaire pour l’Atmosph´ere et l’Astrophysique, Universit´e Pierre et Marie Curie-Paris 6, Paris, France

5Spectroscopie de l’Atmosph`ere, Service de Chimie Quantique et de Photophysique, Universit´e Libre de Bruxelles (U.L.B.), Brussels, Belgium

6Meteorological Observatory Hohenpeißenberg, DWD, Hohenpeißenberg, Germany

7Royal Meteorological Institute of Belgium (R.M.I.B.), Brussels, Belgium

8Richard-Aßmann-Observatorium, DWD, Lindenberg, Germany

9NOAA/ESRL, Boulder, CO, USA

10Department of Applied Physics, Eindhoven University of Technology, Eindhoven, The Netherlands

11Finnish Meteorological Institute, Sodankyl¨a, Finland

12Ozone Layer Monitoring Office, Japan Meteorological Agency, Tokyo, 100-8122 Japan

13Agencia Estatal de Meteorolog´ıa (AEMET), Madrid, Spain

14Met ´Eireann, The Irish Meteorological Service, Valentia Observatory, Cahirciveen, Kerry, Ireland

15Met Office, Exeter, UK

16NASA Goddard Space Flight Center, Wallops Flight Facility, Wallops Island, USA

17Federal Office of Meteorology and Climatology, MeteoSwiss, Aerological Station, Payerne, Switzerland

*now at: Astrium GmbH, Germany

One of the authors, H. De Backer, got lost while the manuscript was prepared for ACPD. This corrigendum is to honor his contribution to this paper.

Correspondence to: M. Eremenko ([email protected])

Published by Copernicus Publications on behalf of the European Geosciences Union.

Références

Documents relatifs

Figure 8: Example of retrieval improvement for humidity profile in Tropics (Paramaribo 2014/10/22) with R iter selection and σ simul for MOC60L (left) and relative error

DQG 7 '1$ OLJDVH EXIIHU SURYLGHG E\ 3URPHJD 7KH\ ZHUH DGGHG LQWR GU\ OLSLG ILOP FRQWDLQLQJ D YDULHW\ RI OLSLG FRPSRQHQWV LQ PJ 7KH OLSLG'1$ PL[WXUHV ZHUHVWURQJO\ YRUWH[HGDQGSXW

(1994) have shown for the Jan-Feb cases with low ozone poleward of 55 ◦ N, when the anticyclone beneath the coldest part of the polar vortex edge develops into a per- sistent

Although in some papers two satellite retrieval algorithms have been compared [e.g., see Mu¨ller et al., 2003], this paper is unique in comparing nine different retrieval

By contrast, we show that large LT ozone columns when not associated with large UT ozone columns but with en- hanced CO total columns – used as a pollution tracer – indi- cate the

Because of the very large amount of IASI data available for 2008, the summarised validation prospect presented here focuses on the measurements that co- locate with

Instrumental method: Gas phase titration (GPT). Comparison of modern surface ozone ob- servations with historical records.. Data selection identified as questionable under

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des