Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 41, Issue 4, Pages 1329-1335Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2013GL058302
Keywords
stable water isotopes; tropical convection; amount effect
Categories
Funding
- Office of Biological and Environmental Research of the U.S. DOE [DE-SC0008679]
- NSF [AGS-1062016, AGS-1260368, AGS-1260380]
- NASA [NNX13AN47G]
- U.S. Department of Energy (DOE) [DE-SC0008679] Funding Source: U.S. Department of Energy (DOE)
- Directorate For Geosciences
- Div Atmospheric & Geospace Sciences [1260380] Funding Source: National Science Foundation
- Directorate For Geosciences
- Div Atmospheric & Geospace Sciences [1062016, 1260368] Funding Source: National Science Foundation
- NASA [NNX13AN47G, 467684] Funding Source: Federal RePORTER
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A stable water isotopologue-enabled cloud-resolving model was used to investigate the cause of the amount effect on the seasonal (or longer) time scales. When the total water (vapor and condensed phase) budget of the precipitating column of air is considered, our results indicate that as convection becomes stronger and the precipitation rate increases, the delta D of precipitation (delta D-p) depends on the isotopic composition of the converged vapor more than that of surface evaporation. Tests with disabled fractionation from rain evaporation demonstrate that this mechanism does not account for the amount effect as has been previously suggested. If the isotopic content of converged vapor is made uniform with height with a value characteristic of surface evaporation, the amount effect largely disappears, further supporting the dominance of converged vapor in changes to the delta D-p signal with increasing precipitation. delta D-p values were compared to the water budget term E/P, where P is precipitation and E is evaporation. Results from this comparison support the overall conclusion that moisture convergence is central in determining the value of delta D-p and the strength of the amount effect in steady state.
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