“Amount effect” of water isotopes and quantitative analysis of post‐condensation processes
By Jung‐Eun Lee, I. Fung. 2008
305 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geochemistry and Petrology, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/c96c9de8cacccc36b010029fd3a89e0c8df3d380
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In Atmospheric Science
In Geochemistry and Petrology
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Citations in the corpus
- Stable water isotopes in the ECHAM5 general circulation model: Toward high‐resolution isotope modeling on a global scale (2011, result): “A number of studies have already clearly demonstrated this possibility of an improved interpretation of detected water isotope variability in terms of climate and environmental change by appropriate GCM simulation results [e.g., Mathieu et al., 2002; Noone and Simmonds, 2002; Werner and Heimann, 200”
- Evaluating hydrological processes in the Community Atmosphere Model Version 5 (CAM5) using stable isotope ratios of water (2017, background): “However, the actual cause of the amount effect remains unclear [Lee and Fung, 2008; Risi et al., 2008; Moore et al., 2014; Conroy et al., 2016].”
- Measuring variations of δ 18 O and δ 2 H in atmospheric water vapour using two commercial laser-based spectrometers: an instrument characterisation study (2012, background): “parametrisations of evaporation (He and Smith, 1999), transpiration (Dongmann et al., 1974) and rainfall re-evaporation (Lee and Fung, 2008).”
- Water-stable isotopes in the LMDZ4 general circulation model: Model evaluation for present-day and past climates and applications to climatic interpretations of tropical isotopic records (2010, methodology): “On the other hand, if the SST change has a lower equator to pole gradient, as simulated by the IPSL or CAM coupled models [Lee et al., 2008], then using the spatial slope for temperature reconstruction leads to an underestimation of past temperature changes (by about 40% in the LMDZ‐iso simulation…”