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Varying soil moisture–atmosphere feedbacks explain divergent temperature extremes and precipitation projections in central Europe

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Academic year: 2020

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Figure 1. Change in (a) TXx and (b) summer precipitation (pre-cip) in Central Europe (CEU, defined in the inset of panel a) for44 model realizations for wet (blue), dry (orange), and very dry(dark red) models and the multi-model median (dashed)
Figure 2. Change in summerradiation (and very dry models (red), and the multi-model median (dashed)
Figure 3. Change incip) in CEU with respect to the base period (1951–1970). Changesare computed based on 20-year moving averages with respect tothe base period
Figure 5. (a) Future vs. present-day cor(TXx, precip) for wet (blue), dry (orange), very dry models (red) and for observations
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