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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 5
Clim. Past, 9, 2173–2193, 2013
https://doi.org/10.5194/cp-9-2173-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 9, 2173–2193, 2013
https://doi.org/10.5194/cp-9-2173-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 Sep 2013

Research article | 16 Sep 2013

Can we determine what controls the spatio-temporal distribution of d-excess and 17O-excess in precipitation using the LMDZ general circulation model?

C. Risi et al.

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Cited articles

Barkan, E. and Luz, B.: High precision measurements of 17O/16O and 18O/16O ratios in H2O, Rapid Commun. Mass Sp., 19, 3737–3742, 2005.
Barkan, E. and Luz, B.: Diffusivity fractionations of H$_2^16$O/H$_2^17$O and H$_2^16$O/H$_2^18$O in air and their implications for isotope hydrology, Rapid Commun. Mass Sp., 21, 2999–3005, 2007.
Barnes, C. and Allison, G.: Tracing of water movement in the unsaturated zone using stable isotopes of hydrogen and oxygen. J. Hydrol, 100, 143–176., 1988.
Barras, V. and Simmonds, I.: Observation and modelling of stable water isotopes as diagnostics of rainfall dynamics over Southeastern Australia, J. Geophys. Res., 114, D23308, https://doi.org/10.1029/2009JD012132, 2009.
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