Modeling atmospheric stable water isotopes and the potential for constraining cloud processes and stratosphere‐troposphere water exchange

By Gavin A. Schmidt, G. Hoffmann, D. Shindell, Yongyun Hu. 2005

195 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/740f9bb4424d9c9c585b075122ab89014cdddac1

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Citations in the corpus

Climate Change Impacts on Plant Pathogens and Plant Diseases (2014, background): “2000), Devon, United Kingdom, and the National Aeronautic and Space Administration Goddard Institute for Space Studies (Schmidt et al. 2005), New York, for the decades of the 2030s, 2050s, and 2080s, which were compared with meteorological data collected between 1955 and 2001 (Salinari et al.”
Stable water isotopes in the ECHAM5 general circulation model: Toward high‐resolution isotope modeling on a global scale (2011, methodology): “It is noteworthy that our new formulation of S is very close, but not identical to the formulation S = 1. � 0.004·Tcond used in the latest isotope version of the LDMZ4 [Risi et al., 2010], CAM2 [Lee et al., 2007], and GISS ModelE [ Schmidt et al., 2005 ] as well as the formulation S = 1. � 0.005·Tco”
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, background): “[29] The parameter l, controlling kinetic effects during snow formation, is known to have a strong impact on the d of snowfall in Antarctica [Jouzel and Merlivat, 1984; Schmidt et al., 2005].”
Role of continental recycling in intraseasonal variations of continental moisture as deduced from model simulations and water vapor isotopic measurements (2013, methodology): “Isotopic processes are represented in a way similar to other isotopic GCMs [Jouzel et al., 1987, 1991; Hoffmann et al., 1998; Noone and Simmonds, 2002; Schmidt et al., 2005; Lee et al., 2007a; Yoshimura et al., 2008; Tindall et al., 2009].”
Historical isotope simulation using Reanalysis atmospheric data (2008, methodology): “[2003] measured slightly different values and produces a deuterium excess 3% systematically higher in the same conditions, but negligible on the variability [Schmidt et al., 2005].”