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Little Ice Age climate reconstruction from ensemble reanalysis of Alpine glacier fluctuations

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Academic year: 2017

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Table 1. Sources of glacier length change data used in this study.
Fig. 1. Comparison of modeled and measured terminus position histories of seven glaciers
Table 2. LV -model parameters of the best-matching DESM: ver- ver-tical elevation difference of the accumulation area Z 0 , bed slope angles of the LV -model β LV , average slope angles of the whole glacier and the ablation area β tot and β abl , the Harri
Fig. 2. ELA variation reconstruction leading to best agreement with length change records from seven glaciers (Fig
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