Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 42, Issue 12, Pages 5042-5050Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GL064117
Keywords
HDO budget; TES; mass balance; closure assumption
Categories
Funding
- National Science Foundation Macrosystems Ecology program [EF-01241286]
- Department of Defense
- NSF Climate and Large Scale Dynamic program as part of a Faculty Early Career Development award [AGS-0955841]
- Center for High Performance Computing at the University of Utah
- Direct For Biological Sciences
- Emerging Frontiers [1241286] Funding Source: National Science Foundation
- Directorate For Geosciences
- Div Atmospheric & Geospace Sciences [1539234] Funding Source: National Science Foundation
- Office of Integrative Activities
- Office Of The Director [1208732] Funding Source: National Science Foundation
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Deuterium to hydrogen (D/H) ratios in Earth's hydrologic cycle have long served as important tracers of climate processes, yet the global HDO budget remains poorly constrained because of uncertainties in the isotopic compositions of continental evapotranspiration and runoff. Here bias-corrected satellite retrievals of HDO and H2O concentrations from the Tropospheric Emissions Spectrometer are used to estimate the marine atmospheric surface layer HDO vapor pressure deficit, from which we calculate the global flux-weighted average oceanic evaporation isotopic composition as -37.6. Using these estimates, combined with D/H ratios in precipitation, global mass balance suggests H isotope compositions for global runoff and terrestrial evapotranspiration of -77.3 and -40.0, respectively. By resolving the HDO budget, we establish an accurate global baseline for geochemically enabled Earth system models, demonstrate patterns in entrainment of moisture into the marine surface layer, and determine the isotopic composition of continental fluxes critical for global ecohydrologic investigations.
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