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Coincidences of climate extremes and anomalous vegetation responses: comparing tree ring patterns to simulated productivity

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Academic year: 2017

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Figure 1. Example of coincidence analysis between a time series of (a) precipitation (P ) and (b) tree ring width indices (TRW)
Figure 2. Histograms of deviations of growth responses of TRW (a, b, c) and NPP (d, e, f) during extreme years in units of standard deviations (z-scores)
Figure 4. Map of coincidence rates between extremes in simulated NPP and precipitation for (a) broadleaved and (b) needle-leaved trees
Figure 6. Significant coincidence rates of TRW (red dots) and sim- sim-ulated NPP at TRW sites (blue dots) with (a) precipitation, (b)  tem-perature, and (c) the combination of both, in climate space (as given in 2.5 ◦ C temperature bins, x axis) averaged
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