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

Combined measurements of the H<sub>2</sub><sup>18</sup>O and HDO isotopic ratios in precipitation, leading to second-order parameter D-excess, have provided additional constraints on past climates compared to the H<sub>2</sub><sup>18</sup>O isotopic ra...

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Bibliographic Details
Main Authors: C. Risi, A. Landais, R. Winkler, F. Vimeux
Format: Article
Language:English
Published: Copernicus Publications 2013-09-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/9/2173/2013/cp-9-2173-2013.pdf