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Gedzekman, Stanley David (2011)
Publisher: Tellus B
Journal: Tellus B
Languages: English
Types: Article
A model for the isotopic composition of water vapor above the atmospheric boundary layer ispresented. The model includes the effects of isotope fractionation and vertical turbulenttransport of vapor. It utilizes an assumed air trajectory in which an air parcel initially acquireswater vapor over the ocean, rises dry and then moist adiabatically. and finally sinks to theobserved conditions of height, temperature and dew point temperature. Discrepanciesbetween model predictions and actual profiles are shown to have characteristic signatureswhich render the isotopic composition of water vapor of potential value as a dynamic tracer ofatmospheric processes and motions.DOI: 10.1111/j.1600-0889.1988.tb00217.x 
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    • research w a s s u p p o r t e d by NSF ATM g r a n t s 81 16371 and 83 13954. Lamont-Doherty G e o l o g i c a l O b s e r v a t o r y of C o l u m b i a U n i v e r s i t y C o n t r i - led t o a m a r k e d i m p r o v e m e n t o f t h e p a p e r . The b u t i o n No. 4198.
    • Covey. C. and Haagenson. 1984. A model of oxygen isotope composition of precipitation : implications for paleoclimatic data. J. Geophys. Res. 83, 0 3 , 4647- 4655.
    • Dansgaard, W. 1953. The abundance of 0 l a in atmospheric water and water vapour. Tellus 5 , 461-469.
    • Dansgaard. W. 1954. The Oi8 abundance in fresh water. Geochim. Cosmochim. Acra 6, 241-260.
    • Dansgaard. W. 1964. Stable isotopes in precipitation. Tellus 16, 436-468.
    • Ehhalt, D. 1974. Vertical profiles of HTO, HDO, and H?O in the troposphere. NCAR Technical Note, NCAR-TN/STR-100, 131 pp.
    • Ehhalt, D., Patz, H.W., Pollock, W., Heidt, L. E. and Lueb, R. 1980. Measurement of atmospheric water vapor by cryogenic collection. In : Atmospheric wuter vapor, A. Deepak. T. D. Wilkerson and L. H. Ruhnke, Eds., Academic Press, 303-314.
    • Eriksson, E. 1965. Deuterium and IBOin precipitation and other natural waters : some theoretical considerations. Tellus 27, 498-512.
    • Facy, L., Merlivat, L., Nief, G. and Roth, R. 1963. The study of formation of hailstones by isotopic analysis. J. Geophys. Res. 68. 3841-3848.
    • Fleagle, R. G . and Businger. J . A. 1980. A n Introduction to Atmospheric Physics. Academic Press, NY, 432 pp.
    • Gedzelman, S. D. and Lawrence, J . R. 1982. The isotopic composition of cyclonic precipitation. J. Appl. Meteorol. 21, 1385- 1404.
    • Jouzel, J . 1979. Teneur isotopique de la vapeur d'eau atmospherique. Mise au point d'un systeme embarquable. J . Rech. Atmos. 13, 261-269.
    • Jouzel, J . and Merlivat, L. 1984. Deuterium and oxygen-I8 in precipitation: modeling of the isotopic effects at snow formation. J . Geophys. Res. 80,5015- 5030.
    • Knight, C. A.. Knight, N . C . and Kime, K . A. 1981. Deuterium content of storm inflow and hailstone growth layers. J . Armos. Sci. 38, 2485-2499.
    • Liu, S. C., McAfee, J. R. and Cicerone, R. J. 1984. Radon 222 and tropospheric vertical transport. J. Geophys. Res. 89. 0 5 , 7291-7297.
    • Majoube, M. 1971. Fractionation of oxygen 18 and of deuterium between water and its vapor (in French). J. Chim. Phys. 68, 1423-1436.
    • Mason, B. J . 1971. The physics of clouds, 2nd edition. Oxford University Press, NY, 671 pp.
    • Merlivat, L. and Jouzel, J. 1979. Global climatic interpretation of the deuterium-oxygen I8 relationship for precipitation. J . Geophys. Res. 84, 5029- 5033.
    • Merlivat, L. and Nief, G . 1967. Isotopic fractionation of the solid-vapor and liquid-vapor changes of state of water at temperatures below 0°C (in French). Tellus 19, 122-127.
    • Miyake, Y., Matsubaya, 0.and Nishihara, C. 1968. An isotopic study on meteoric precipitation. Pup. Meteorol. Geophys. 19, 243-266.
    • Pollock, W., Heidt, L. E., Leub, R. and Ehhalt. D. H . 1980. Measurement of stratospheric water vapor by cryogenic collection. J . Geophys. Res. 85, 5555-5568.
    • Pruppacher, H . R. and Klett, J. D. 1980. Microphysics of clouds and preripitaiion. D. Riedel Pub. Co., Dordrecht, Holland, 714 pp.
    • Rozanski, K. and Sonntag, C. 1982. Vertical distribution of deuterium in atmospheric water vapor. Tellus34, 135-141.
    • Rozanski, K., Sonntag, C. and Munnich, K . 0. 1982. Factors controlling stable isotope composition of European precipitation. Tellus 34, 142-150.
    • Taylor, C. B. 1972. The vertical variations of the isotopic concentrations of tropospheric water vapour over continental Europe and their relationship to tropospheric structure. N.Z. Dep. Sci. Ind. Res., Inst. Nucl. Sci., Rep. INS-R-107, 44 pp.
    • Taylor, C. B. 1984. Vertical distribution of deuterium in atmospheric water vapour : problems in application to assess atmospheric models. Tellus 368, 67-72.
    • White, J . W. C. and Gedzelman, S. D. 1984. The isotopic composition of atmospheric water vapor and the concurrent meteorological situation. J. Geophys. Res. 89, 0 3 , 49374939.
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