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Original Articles

Détermination des flux de vapeur d'eau entre la couche limite planétaire et l'atmosphère libre

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Pages 552-561 | Received 22 Jul 1974, Accepted 28 Apr 1975, Published online: 15 Dec 2016

Bibliographie

  • Ball, F. K. 1970. Control of inversion height by surface heating. Quart. J. Roy. Met. Soc. 86, 483.
  • Bean, R. B., Gilmer, R., Grossman, R. L. and Mc-Gavin, R. 1972. An analysis or airborne meas-urements of vertical water vapor flux during Bomex. J. Atmos. Sci. 29, 860–869.
  • Browning, K. A., Starr, J. R. and Whyrnan, A. J. 1973. The structure of an inversion above a con-vective boundary layer as observed during high-power pulsed doppler radar. Boundary Layer Meteorol. 4, 91.
  • Donelan, M. and Miyake, M. 1973. Spectra and fluxes in the boundary layer of the trade-wind zone. J. Atmos. Sci. 30, 444–464.
  • Druilhet, A. and Fontan, J. 1972. Determination des coefficients de diffusion turbulente entre 0 et 100 m a Paide du Rn et du ThB. Boundary Layer Meteorol. 3, 476.
  • Druilhet, A. and Fontan, J. 1973. Utilisation du tho-ron pour la determination des coefficients de dif-fusion turbulente pres du sol. Tellus 25 (2), 199–212.
  • Dyer and Maher, 1965. Automatic eddy flux meas-urement with the evaporation J. Appl. Meteorol. 4, 622.
  • Guedalia, D., Birot, A., Fontan, J. and Allet, C. 1971. Sur la determination des coefficients de diffusion dans is couche limite planétaire a l'aide du Rn et du ThB. C.R. Acad. Sci., Paris, 273, 57.
  • Guedalia, D., Allet, C., Fontan, J., Druilhet, A. and Assaf, G. 1973. Lead-212, Rn and vertical mix-ing in the lower atmosphere (100-2 000 m). Tellus 25 (4), 381–385.
  • Guedalia, D., Allet, C. and Fontan, J. 1974a. Vertical exchange measurements in the lower troposphere using ThB and radon. J. Applied Meteorol. 13 (1), 27-39.
  • Guedalia, D., Druilhet, A. and Fontan, J. 1974b. Determination des échanges verticaux moyens dans la C.L.P. a partir des données statistiques obtenues par lea radiosondages de temperature. Boundary Layer Meteorol. 7, 457.
  • Metcalf, J. I. and Atlas, D. 1973. Microscale ordered motions and atmosphere structure associated with thin echo layers in stably stratified zones. Boundary Layer Meteorol. 4, 7.
  • Miyake, M. and McBean, G. 1970. On the measure-ment of vertical humidity transport over land. Boundary Layer Meteorol. 1, 88.
  • Miyake, M., Donelan, M., McBean, G., Paulson, C., Baogley, F. and Leavitt, E. 1970. Comparison of turbulent fluxes over water determined by profile and eddy correlation techniques. Quart. J. Roy. Meteorol. Soc. 96, 132–137.
  • Oke, T. R. 1970. Turbulent transport near the ground in stable conditions. J. Appl. Meteorol. 9, 778.
  • Pond, S., Phelps, G. T., Paquin, J. E., McBean, G. and Stewart, R. W. 1971. Measurements of the turbulent fluxes of momentum, moisture and sensible heat over the ocean. J. Atmos. Sci. 28, 901–917.
  • Puech, J. and Hernandez, M. 1973. Evapotranspira-tion comparée de différentes cultures et etude de quelques facteurs influencant lea rythmes de consommation. Annales agronomiques, Paris, 24 (4), 437–455.
  • Readings, C. J., Golton, E. and Browning, K. A. 1973. Fine-scale structure and mixing within an inversion. Boundary Layer Meteorol. 4, 275.
  • Saissac, J., Dampierre, F. and Mercusot, C. 1971. Sur le nombre de Richardson dans les échanges verticaux de la couche imite. C.R. Acad. Sci., Paris, 272, B, p. 1393.
  • Warner, J. 1971. Observations of the eddy fluxes of heat and vapour over the sea. Quart. J. Royal Meteorol. Soc. 97, 540–547.
  • Webb, E. K. 1970. Profile relationships: the log. linear range and extension to strong stability. Quart. J. Roy. Met. Soc. 96, 67.
  • Wilson, R. G. and Rouse, W. R. 1972. Moisture and temperature limits of the equilibrium evapo-transpiration model. J. Appl. Meteorol. 11, 436.
  • Yelagina, L. G. and Koprov, B. M. 1971. Measure-ment of turbulent humidity flux and their fre-quency spectra. lzv. Atm. and Oceanics Physics 7 (2), 115.
  • Zobel, R. F. 1966. Temperature and humidity changes in the lowest few thousand feet of the atmosphere during a fine summer day in South-ern England. Quart. J. Roy. Meteorol. Soc. 92, 196.