[1] Chong, M. « Mesure des profils de vent par sodar-doppler », Note Technique CRPE/22, 1976 103 p.
[2] Aubry, M., R. Chezlemas, A. Spizzichino, “Preliminary Results of the Atmospheric Acoustic Sounding Program at CNET”, Boundary Layer Meteorol., 1974, 7, p. 513-319.
[3] Spizzichino, A., “Discussion of the Operating Conditions of a Doppler Sodar”, J. Geophys. Res., 1974, 79, 36, p. 5585-5591.
[4] Spizzichino, A., “A spectral acoustic and radio waves scattered by atmospheric turbulence in the case of radar and sodar experiments”, Ann. Geophys., 1975, 31, 4, p. 433- 445.
[5] Estival, A. and Aubry, M, « Interprétation des échos sodar en termes de stratifications atmosphériques », La Météorologie VI, 1975, 5, p. 33–42.
[6] Weill A., M. Aubry, F. Baudin, J. Heissat, “a study of temperature fluctuations in the Atmospheric Boundary Layer”, Boundary Layer Meteorol., 1976, 10, 3, p. 337- 346.
[7] Kaynejad Mahomed, « mesure du taux de dissipation turbulent », thèse de Docteur- Ingénieur, Paris VI., 1975.
[8] Weill A., W. Brandes, C. Oberto and P. Bares, « Anémomètre à fil chaud embarquable sur ballon captif » J. Phys. Colloques 37, 1976, C1-173-C1-175 DOI: 10.1051/j.phys.,976125.
[9] Weill, A., Baudin, F., P. Van Grunderbeeck, P. Leberre, “turbulence structure in temperature inversion and in convection fields as observed by Doppler Sodar”, Boundary Layer Meteorol., 1976, 10, 3, p. 337-346.
[10] Eymard Laurence, Thèse de troisième cycle : « ondes de gravité dans la couche limite planétaire : étude par sondage acoustique », Université de Paris VI, 1978.
[11] Van Grunderbeeck Patrick, thèse de troisième cycle : «Etude de la détermination des profils atmosphériques de température et humidité par sondage acoustique multifréquence», Université de Paris VI, 1976.
[12] Van Grunderbeeck P., « Etude de la détermination des profils atmosphériques de température et humidité par sondage acoustique multi-fréquence », la Météorologie, 1975,12, p. 51-69
[13] Eymard, L. and A. Weill, “A study of gravity waves in the boundary layer by acoustic sounding”, Boundary-Layer Meteorol., 1979, 17, 2, p. 231–245.
[14] Strauss B., « Estimation du bilan d’énergie cinétique turbulent par sondage acoustique ». Document de travail CRPE, 1980, N° 1063.
[15] André, J. C., De Moor, G., Lacarrère, P., Therry, G., and du Vachat, R.: 1978, “Modeling the 24-Hour Evolution of the Mean and Turbulent Structures of the Planetary Boundary Layer”, J. Atmos. Sci., 1978, 35, p. 1861–1885.
[16] Weill A., L. Eymard, M.E. Lequere, C. Klapisz, F. Baudin, and P. Van Grunderbeeck, “Investigation of the planetary boundary layer with an acoustic sounder”, in Proceedings of the IVth symposium on ‘meteorological observations’, 1978, Denver, AMS, p. 415-421.
[17] Weill A, Klapisz C, Strauss B, Baudin F, Jaupart C, Van Grundeerbeeck P and Goutorbe J. P. 1980 “Measuring heat flux and structure functions of temperature fluctuations with an acoustic Doppler sodar”, J. Appl. Meteorol., 1980, 19, p. 199–205.
[18] Taconet Odile, « Propriétés et structure des cellules convectives dans la couche limite atmosphérique par sondage acoustique Doppler », thèse de 3ème cycle, Paris XI, 25 mars 1980.
[19] Taconet O., A. Weill, “Convective plumes in the atmospheric boundary layer as observed with an acoustic Doppler sodar”, Boundary Layer Meteorol., 1982, 25, p.143-158.
[20] Taconet, O. and A. Weill, “Vertical Velocity Field in the Convective Boundary Layer as Observed with an Acoustic Doppler Sodar”, Boundary-Layer Meteorol, 1983, 23, p.133–151.
[21] Van Grunderbeeck, P., Leberre, P., Weill, A., Dubosclard, G., and Itier, B, « Mouvements convectifs de la couche limite atmosphérique observés au moyen de sondeurs acoustiques Doppler et d'instruments portés par un ballon captif », Compt. Acad. Sci. Paris, 1979, 288, p. 209–212.
[22] Dubosclard G., “A comparison between observed and predicted values for the entrainment coefficient in the planetary boundary layer”, Boundary Layer Meteorol., 1980, 18, p. 473 – 483.
[23] Klapisz, C., A. Weill, “Mean horizontal wind in inversion-capped convective boundary layer”, J. Appl. Meteor., 1982, 21(5), p. 648-655.
[24] Weill A., D. Vidal-Madjar, C. KLAPISZ, J.P. GOUTORBE, « La couche limite hivernale, Journée d'Evry, colloque environnement », 1980.
[25] Louis, J.F., A. Weill, and D. Vidal-Madjar, “Dissipation length in stable layers”, Boundary Layer Meteorol., 1983, 25(3), p. 229-243.
[26] Mon, J.P., A. Weill, and L. Martin, “Effect of tropospheric disturbances on a 4.1 and 6.2 GHz line of sight path”, Ann. Télécomm.,1980, 35, (11-12), p. 468-471.
[28] Sommeria G. and J. Testud, “COPT 81: A Field Experiment Designed for the Study of Dynamics and Electrical Activity of Deep Convection in Continental Tropical Regions”, Bulletin of the American Meteorological Society,1984,65,1, p. 4-10.
[29] Dubosclard Georges (1986), Thèse d'Etat, IOPG (Institut Observatoire de Physique du Globe de Clermont-Ferrand.
[30] Weill, A., F. Baudin, C. Mazaudier, G. Desbraux, C. Klapisz, J, P. Goutorbe, A,G.M.Driedonks, A. Druilhet, and M. Durand, “A mesoscale shear convective organization observed during COAST experiment: Acoustic sounder measurements”, Bound. Layer Meteorol.,1988, 44(4), p. 359-371.
[31] Weill, A., C. Klapisz, and F. Baudin, “The CRPE minisodar: Applications in micrometeorology and in physics of precipitation”. Atmos. Res., 1983, 20, p. 317–335.
[32] Coulter, R. L., and T. L. Martin, “Results from a high power, high frequency sodar”, Atmos. Res.,1986, 20, p. 257–270.
[33] Coulter R.L., T. J. Martin, and T. M. Weckwerth, “Minisodar measurements of rain”, J. Atmos. Oceanic Technol., 1989, 6, p. 369–377.
[34] Desbraux Georges, « climatologie dynamique de la turbulence dans la couche limite atmosphérique durant l'experience COAST 83, étude statistique à partir de sondages acoustiques », Université de Clermont-Ferrand, 1985.
[35] Desbraux, G. and A. Weill, “Mean turbulent properties of the stable boundary layer observed during the COAST experiment”. Atmos. Res., 1986, 20, p. 151-164.
[36] Weill A., C. Mazaudier, F. Baudin, C. Klapisz F. Leca, M. Masmoudi, D. Vidal Madjar, R. Bernard, O. Taconet, B.S. Gera, A. Sauvaget, A. Druilhet, P. Durand, J. . Caneil, P. Mery, G. Dubosclard, A. C. M. Beljaars, W. A. Monna, J. G. Van Der Vliet, M. Crochet, D. Thomson, T. Carlson, “The Mesogers 84 experiment: a report”, Boundary Layer Meteorol. ,1988, 42,3, p. 251–264.
[37], Zhong Ming. Thèse à l’Université de Paris VI. Estimation du rayonnement pendant les situations nuageuses de beau temps de MESOGERS 84, 1991.
[38] Zhong, M., A. Weill, and O. Taconet, “Estimation of net radiation and surface heat fluxes using NOAA-7 satellite infrared data during fair-weather cloudy situations of Mesogers-84 experiment” Boundary Layer Meteorol.,1990, 53, 4, p. 353–370.
[39] Masmoudi Mohamed, Thèse université de Paris VI, Etude de l'écoulement à moyenne échelle au cours de l'expérience Mésogers 84, 1988.
[40] Masmoudi M. and A. Weill, “Doppler sodar measurement of atmospheric mesoscale spectra: The Taylor hypothesis analysis” J. Climate Appl.Meteor., 1988, 27, (7), p. 864- 873.
[41] Gera B.S., A. Weill, “Doppler sodar analysis of the frontal friction in relation to the frontal slope” J. Climate Appl. Meteor., 1987, 26 (8), p. 885-891.
[42] Gera B.S. and A. Weill, “Doppler Sodar observations of the boundary-layer parameters and a frontal system during the “Mesogers 84” experiment”, Boundary Layer Meteor., 1991,54, 1-1, p. 41-57.
[43] Soares J.V., R Bernard, O Taconet, D Vidal-Madjar, A Weill, “Estimation of bare soil evaporation from airborne measurements”, Journal of hydrology, 1988, 99 (3-4), p. 281-296.
[44] Weill A., “Indirect measurement of fluxes using Doppler Sodar”. In Land Surface Evaporation: measurement and parametrization, (T. Schmugge and J.C. André Editors), 1991, p. 301-311.
[45] Andre J.C., J.P. Goutorbe, A. Perrier, F. Becker P. Bessemoulin, et al., “Evaporation over land-surfaces: First results from HAPEX-MOBILHY special observing period”. Ann.Geophysicae, European Geosciences Union, 1988, 6, p.477-492. <hal-01011981>.
[46] Mazaudier C., J. Bouvet and A. Weill, “Sodar wind speed profiles over forested boundary layer during the Hapex – Mobilhy campaign”, Ann. Geophysicae, 1991, 9(8), p. 501-509.
[47] Parlange M.B. and W. Brutsaert, “Are radiosonde time scales appropriate to characterize boundary layer wind profiles”, J. Appl. Meteorol.,1990, 29, 3, p. 249-255.
[48] Weill A. and H.R. Lehmann, “twenty years of acoustic sensing: a review and some applications”, Z. Meteorol., 40(4), 1990, p. 241-250.
[49] Kotroni V. and Amory-Mazaudier, C., “Influence of orographic and canopy conditions on friction velocities observed during frontal events using Doppler sodar observations”. J. Appl. Meteorol., 1993, 32, p. 506-521.
[50] Kotroni V., C. Amory-Mazaudier, K. Lagouvardos, “Doppler Sodar observations of a cold front during Pyrex Experiment: orographic aspects”, Int. J. Remote Sensing, 1994, 15, 2, p. 489-497.
[51] Beyrich F. and A. Weill, “Some aspects of determining the stable boundary layer depth from sodar data” Boundary-Layer Meteorol, 1993, 63, 1-2, p. 97–116.
[52] Weill A., G. Brandeis, S. Vergniolle, F. Baudin, J. Bilbille, J.F. Fèvre, B. Piron and X. Hill, “Acoustic sounder measurements of the vertical velocity of volcanic jets at Stromboli volcano”, Geophys. Res. Lett., 1992, 19, p. 2357-2360.
[53] Brandeis, G., ‘’ faudra-t-il un jour évacuer Naples? La dynamique des volcans’’, La Recherche, 1995, 274, p. 301-304.
[54] Dubosclard G., R. Cordesses, P. Allard, C. Hervier, M. Coltelli and J. Kornprobst, “First Testing of a Volcano Doppler Radar (Voldorad) at Mount Etna, Italy’’, Geophys. Res. Lett ,1999, 26, 22, p. 3389-3392.













