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Romaroson, R.. et al., A box model for on-line computations of diurnal variations in a 1D model: potential application un multidimensional cases. An. Geophysicae, 10, 416-418, 1992. Rothman, L.S. et al., The HITRAN 2004 molecular spectroscopic database. J. Quant.Spec.Rad. Trans., 96(2), 139-204, 2005. Selkirk,H.B., The tropopause cold trap in the Australian monsoon during STEP/AMEX 1987, J. Geophys. Res., 98(D5), 8591-8610, 1993 Sen, B. et al., The budget and partitioning of stratospheric chlorine during the 1997 Arctic summer, J. Geophys. Res., 104, D21,26653 Schauffler , S.M. et al., Chlorine budget and partitinning during the Stratospheric Aerosol and Gas Experiment (SAGE III) Ozone loss and Validation Experiment (SOLVE). J. Geophys. Res., 108(D5), 4173, 2003. Schoeberl, M.R. et al., An estimation of the dynamical isolation of the tropical lower stratosphère using UARS wind and trace gas observations of the quasibiennal oscillation, Geophys. Res. Lett., 24, 53-56, 1997. Shapiro,M.A., Further evidence of the mesoscae and turbulent structure of upper level jet stream-frontal zone systems.Min.Wea.Rev.,106,1100-111,1978 Sharpe, S. W. et al. Gas-Phase Databases for Quantitative Infrared Spectroscopy, Appl. Spectrosc. 58, 1452-1461, 2004. Sivakumar, V. et al., Tropopause characteristics over southern tropical site, Reunion Island (21°S, 55°E) ; Using radiosonde-ozonesonde data, J. Geophys. Res.,111, D19111, 2005. Sofieva, V.F. et al., Spatio-temporal observations of the tertiary ozone maximum, Atmos. Chem. Phys., 9, 4439-4445, 2009. Spaete,P. et al., Stratospheric-tropospheric mass exchange during the President’s Day Storm, Mon. Weather Rev., 122, 424-439, 1994. Schoeberl, M.R., et al., QBO and annual cycle variations in tropical lower stratosphere trace gases from HALOE and Aura MLS observations. J. Geophys. Res., 113(D5), 1-15., 2008. Solomon, S. et al., Time-dependant ozone depletion potentials for short-and long-term forecasts, nature, 357 (6373),33-37, 1992. Steck, T. et al., Retrieval of global upper tropospheric and stratospheric formaldehyde (H2CO) distributions from high-resolution MIPAS-Envisat spectra, Atmos. Chem. Phys., 8, 463–470, 2008. Stohl, A., et al., Stratosphere-troposphere exchange: A review, and what we have learned from STACCATO. J. Geophys. Res., 108(D12), STA 1-1 - STA 1-15, 2003. 107
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UNIVERSITÉ D’ORLÉANS ÉCOLE DOC
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Il y a une personne qui n’a pas e
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CHAPITRE 3 SIMULATION ET INVERSION
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prépondérant. Cependant, les mesu
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CHAPITRE 1 CONTEXTE SCIENTIFIQUE A)
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Figure 1-1 - Profil vertical de tem
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∂θ est le terme de stabilité st
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A.2.2 Circulation stratosphérique
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adiatif de cette couche et agissent
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et 3.5 PVU (Hoerling et al., 1991),
Page 21 and 22:
Il est utile de mentionner que les
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trillion in volume » : pptv). Tout
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Les principales sources de chlore s
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CCl4 ou le méthyl chloroforme CH3C
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Figure 1-7 - Distributions latitudi
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Parallèlement aux mesures satellit
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cette estimation. Ainsi, ces désac
Page 35 and 36:
HO2 + ClO → HOCl + O2 (1.25) HOCl
Page 37 and 38:
CHAPITRE 2 MESURES DE COMPOSES ATMO
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de 0.8 μm à 2.5 μm environ, l’
Page 41 and 42:
- Elargissement naturel: Il trouve
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g ( % ν ) = g ( % ν ) ⊗ g ( %
Page 45 and 46:
2.2. Description de l’instrument
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diode est refroidi à l’azote liq
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d’échelle de nombre d’onde) a
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Pour étalonner de manière absolue
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en particulier de la fonction d’a
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Figure 2-10 - Procédure d’ajuste
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CHAPITRE 3 SIMULATION ET INVERSION
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d’absorption attendus pour chaque
Page 62 and 63: Figure 3-3 - Profil vertical de rap
Page 64 and 65: Figure 3-5 - Raies d’absorption d
Page 66 and 67: du choix. Notons que La raie à 283
Page 68 and 69: mesure correcte de formaldéhyde re
Page 70 and 71: 3.2.4 Etalonnage des raies d’abso
Page 72 and 73: Nous trouvons donc un bon accord en
Page 74 and 75: Le premier vol de SPIRALE en régio
Page 76 and 77: On constate que des valeurs de temp
Page 78 and 79: Figure 3-14 - Profils verticaux de
Page 80 and 81: du second vol tropical de SPIRALE,
Page 82 and 83: Dans ce chapitre, nous abordons l
Page 84 and 85: Figure 4-3- Ajustement de la raie d
Page 86 and 87: Altitude (m) p 33000 31000 29000 27
Page 88 and 89: Figure 4-7 - Rétro-trajectoires de
Page 90 and 91: 4.2.2. Mesures de HCl dans la basse
Page 92 and 93: Altitude (m) p 33000 31000 29000 27
Page 94 and 95: SPIRALE, 22 Juin 2005 Easterly Alti
Page 96 and 97: mélange de (a) HCl (en unité de 0
Page 98 and 99: Le 9 Juin 2008, entre 15 et 20 km d
Page 100 and 101: géographiques au voisinage de cell
Page 102 and 103: Niveaux de pression (hPa) N# de poi
Page 104 and 105: sont révélées être inférieures
Page 106 and 107: soumettre au journal de l’Europea
Page 108 and 109: Références bibliographiques Appen
Page 110 and 111: Hauchecorne, A., et al., Quantifica
Page 114 and 115: Annexe: Publication parue dans le j
Page 116 and 117: 1 Introduction Active chlorine spec
Page 118 and 119: FTS satellite instrument in agreeme
Page 120 and 121: absorption signal is difficult to r
Page 122 and 123: found at an almost constant value o
Page 124 and 125: our previous paper (Moreau et al.,
Page 126 and 127: PV fields on isentropic surfaces. T
Page 128 and 129: Between 46.4 hPa and 10.0 hPa (i.e.
Page 130 and 131: As a conclusion, the present paper,
Page 132 and 133: Folkins, I., Loewenstein, M., Podol
Page 134 and 135: Version 2.2 level 2 data quality an
Page 136 and 137: Rothman, L. S., Jacquemart, D., Bar
Page 138 and 139: F., Höpfner, M., Huret, N., Jones,
Page 140 and 141: Fig. 2. Vertical profiles of temper
Page 142 and 143: Altitude (m) 31000 29000 27000 2500
Page 144 and 145: Fig. 6. Latitudinal and longitudina
Page 146 and 147: (a) Pressure (hPa) (b) Pressure (hP
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