Abstract
The isotopic content of precipitation falling at a point provides information of potential importance concerning atmospheric circulation and climate change1–6. The isotopic content of precipitation, however, is controlled by the particular meteorological processes acting at a given time and place and is subject to considerable variation. We have measured the deuterium-to-hydrogen ratios (D/H) of precipitation at Mohonk Lake, New York, from individual storms over a 2-yr period, July 1977–June 1979. These ratios varied systematically with the locus of the paths followed by the storms: the more seawards (and southerly) the paths and the colder the temperatures at Mohonk, the lower were the D/H ratios.
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Lawrence, J., Gedzelman, S., White, J. et al. Storm trajectories in eastern US D/H isotopic composition of precipitation. Nature 296, 638–640 (1982). https://doi.org/10.1038/296638a0
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DOI: https://doi.org/10.1038/296638a0
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