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final result to the favored altitudinal distribution (either from SAFRAN or from the model)
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and to SAFRAN’s extrapolation over higher altitudes where weather stations are scarcer.
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## Analogue days
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Then for the moment, we have presented a methodology that works to construct a forcing over the period common to both initial datasets (SAFRAN and CPRCM run). However, here we introduce another method based on analogue days, which would allow to extend the methodology to the full period covered by SAFRAN (1979-2014). |
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