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- W1978362011 abstract "The relationship between δD and δ18O values (per mille deviation from SMOW) was investigated on falling snow particles from a separate convective cloud collected at 2 stations along a moving cloud trajectory. Observations were made in 1983 in Hokuriku, Japan and in 1985 and 1986 in Hokkaido, Japan. The δD and δ18O values of snow particles from a separate cloud were linearly related. The values of deuterium excess of observed δD-δ18O lines were much greater than 10 and differed with each case, while the slope was 8.5-9.6 in 7 of 9 cases.Such observational results indicated that falling snow particles observed at both stations were produced in a cloud consisting of the air parcels containing initial water vapor having the same isotopic composition and that there was a possibility of kinetic effect in the sublimation process during growth of snow crystals." @default.
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- W1978362011 date "1988-01-01" @default.
- W1978362011 modified "2023-10-17" @default.
- W1978362011 title "Relationship between δD and δ<sup>18</sup>O values of falling snow particles from a separate cloud" @default.
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- W1978362011 doi "https://doi.org/10.3402/tellusb.v40i3.15907" @default.
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