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Vertical distribution of deuterium in atmospheric water vapour.

Tellus (1982) 34(2) 135-141
DOI: 10.3402/tellusa.v34i2.10795
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Abstract

The observed deuterium increase near the tropopause is proposed to be at least partly due to downward mixing of isotopically heavy water vapour produced by methane decomposition in the upper atmosphere. -from Authors

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APA

Rozanski, K., & Sonntag, C. (1982). Vertical distribution of deuterium in atmospheric water vapour. Tellus, 34(2), 135–141. https://doi.org/10.3402/tellusa.v34i2.10795

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