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

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Table 1. Precipitation 17O-excess simulated by LMDZ, compared to data from (Luz and Barkan, 2010) collected in precipitation or rivers.We did not select lakes, caves or ponds in order to avoid samples affected by re-evaporation after rainfall
Table 2. Precipitation 17O-excess simulated by LMDZ, compared to various additional measurements done at LSCE.
Table 3. LGM minus present-day difference in precipitation δ18O, d-excess and 17O-excess in Antarctica observed in ice cores and simulatedby LMDZ.
Fig. 2. Zonal mean of simulated d-excess (a) and 17O-excess (b)in water vapor as a function of latitude and altitude in the SouthernHemisphere.
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