Ocean isotopic evaporation models, such as the Craig‐Gordon model, rely on the description of nonequilibrium fractionation factors that are, in general, poorly constrained. To date, only a few gradient‐diffusion type measurements have been performed in ocean settings to test the validity of the commonly used parametrization of nonequilibrium isotopic fractionation during ocean evaporation. In this work, we present 6 months of water vapor isotopic observations collected from a meteorological tower located in the northwest Atlantic Ocean (Bermuda) with the objective of estimating nonequilibrium fractionation factors (
The Role of Ozone Vibrational Resonances in the Isotope Exchange Reaction 16 O 16 O + 18 O → 18 O 16 O + 16 O: The Time-Dependent Picture
- Award ID(s):
- 1806915
- NSF-PAR ID:
- 10170499
- Date Published:
- Journal Name:
- The Journal of Physical Chemistry A
- Volume:
- 123
- Issue:
- 36
- ISSN:
- 1089-5639
- Page Range / eLocation ID:
- 7733 to 7743
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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