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B. Table, 1: Station locations in the CNIP network the shape of the east-west ? 18 O transect shown on Figure B

B. Figure, 3 shows the discripancies between ? 18 O simulated by REMO iso and CNIP observations Although being qualitatively correct, REMO iso underestimates quantatively the isotopic gradients. We suggest that the overestimation of ? 18 O at high altitudes/latitudes is primarily related to the initial conditions. Soil moisture and snow layer in REMO are initialised at ? 18 O =0 ? / ?? , and the 3-month spin-up is too short to reach an equilibrium with atmospheric processes

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C. Figure, Comparison of monthly precipitation amounts (A ?upper panel) and ? 18 O (B ? lower panel) between REMO iso and GNIP stations. The GNIP station across Australia are located in Adelaide

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