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- W1965916134 abstract "Jouzel and Merlivat developed and used an expression for the kinetic fractionation coefficient α k , and greatly improved the predictions of δ ( 18 O) and d (the deuterium excess) for East Antarctica. The α k coefficient is re-derived in terms of ambient cloud temperatures and is used to re-calculate their single-source East Antarctic simulations. While the “improved” α k produces virtually no change in the δ s , there is a small change in predicted d's. However, no matter which α k is used, the simulated d 's are very sensitive to the supersaturation history of the precipitating air mass. The single-source model is run for a wide range of supersaturation histories. Averaging the resulting suite of δ ( 18 O) and d , solutions gives reasonable and stable d predictions. The temperature T s at which clouds switch from being supercooled water drops to ice crystals depends in part on the microparticle loading of the air. The value of T s significantly influences the d 's and even δ's predicted. Thus ice-core microparticles, d and δ might be “process related”. DOI: 10.1034/j.1600-0889.1991.t01-4-00006.x" @default.
- W1965916134 created "2016-06-24" @default.
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- W1965916134 date "1991-01-01" @default.
- W1965916134 modified "2023-10-14" @default.
- W1965916134 title "Remarks on the deuterium excess in precipitation in cold regions" @default.
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- W1965916134 doi "https://doi.org/10.3402/tellusb.v43i5.15414" @default.
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