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    Original Research Papers

    The origin of Antarctic precipitation: a modelling approach

    Authors:

    Gilles Delaygue ,

    Laboratoire des Sciences du Climat et de l’Environnement (LSCE), FR
    About Gilles
    Additional affiliation: Centre Européen de Recherche et d’Enseignement en Ge´oscience de l’Environnement (CEREGE), Europô le de l’Arbois BP 80, 13545 Aix-en-Provence Cedex 4, France.
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    Valérie Masson,

    Laboratoire des Sciences du Climat et de l’Environnement (LSCE), FR
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    Jean Jouzel,

    Laboratoire des Sciences du Climat et de l’Environnement (LSCE), FR
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    Randal D. Koster,

    Hydrological Sciences Branch, Laboratory for Hydrospheric Processes, US
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    Richard J. Healy

    Marine Chemistry & Geochemistry, US
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    Abstract

    The contribution of different moisture sources to Antarctic precipitation for present-day and glacial conditions is estimated with the NASA/GISS Atmospheric General Circulation Model. Despite its low horizontal resolution (8°×10°), this model simulates reasonably well the broad features of the observed present-day hydrological cycle. Simulated present-day Antarctic precipitation is dominated throughout the year by moisture from a subtropical/midlatitude band (30°S-60°S). The moisture supplied to a given coastal area of Antarctica originates mostly in the adjacent oceanic basin; closer to the pole, other oceanic basins can also contribute significantly. Replacing the present-day sea surface temperatures (SSTs) and sea ice cover in the GCM with those from the CLIMAP oceanic reconstruction for the last glacial maximum (LGM), greatly increases the simulated latitudinal temperature gradient, with the consequence of slightly enhancing the contribution of low latitude moisture to Antarctic precipitation. It also changes the seasonality of the different contributions and thus their budget, particularly in coastal regions. Because the nature of LGM tropical SSTs is still under debate, we performed an additional LGM simulation in which the tropical SSTs are reduced relative to those of CLIMAP. The resulting decrease in the latitudinal gradient brings the relative contributions to Antarctic precipitation more in line with those of the present-day simulation.

    How to Cite: Delaygue, G., Masson, V., Jouzel, J., Koster, R.D. and Healy, R.J., 2000. The origin of Antarctic precipitation: a modelling approach. Tellus B: Chemical and Physical Meteorology, 52(1), pp.19–36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079
      Published on 01 Jan 2000
    Peer Reviewed
     CC BY 4.0

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    Delaygue, G., Masson, V., Jouzel, J., Koster, R.D. and Healy, R.J., 2000. The origin of Antarctic precipitation: a modelling approach. Tellus B: Chemical and Physical Meteorology, 52(1), pp.19–36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079

    Delaygue G, Masson V, Jouzel J, Koster RD, Healy RJ. The origin of Antarctic precipitation: a modelling approach. Tellus B: Chemical and Physical Meteorology. 2000;52(1):19–36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079

    Delaygue, G., Masson, V., Jouzel, J., Koster, R. D., & Healy, R. J. (2000). The origin of Antarctic precipitation: a modelling approach. Tellus B: Chemical and Physical Meteorology, 52(1), 19–36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079

    1. Delaygue G, Masson V, Jouzel J, Koster RD, Healy RJ. The origin of Antarctic precipitation: a modelling approach. Tellus B: Chemical and Physical Meteorology. 2000;52(1):19-36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079

    Delaygue G and others, ‘The Origin of Antarctic Precipitation: A Modelling Approach’ (2000) 52 Tellus B: Chemical and Physical Meteorology 19 DOI: http://doi.org/10.3402/tellusb.v52i1.16079

    Delaygue, Gilles, Valérie Masson, Jean Jouzel, Randal D. Koster, and Richard J. Healy. 2000. “The Origin of Antarctic Precipitation: A Modelling Approach”. Tellus B: Chemical and Physical Meteorology 52 (1): 19–36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079

    Delaygue, Gilles, Valérie Masson, Jean Jouzel, Randal D. Koster, and Richard J. Healy. “The Origin of Antarctic Precipitation: A Modelling Approach”. Tellus B: Chemical and Physical Meteorology 52, no. 1 (2000): 19–36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079

    Delaygue, G, et al.. “The origin of Antarctic precipitation: a modelling approach”. Tellus B: Chemical and Physical Meteorology, vol. 52, no. 1, 2000, pp. 19–36. DOI: http://doi.org/10.3402/tellusb.v52i1.16079

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