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On the Ecology of Mountainous Forests in a Changing Climate: A ...

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134 Chapter 5<br />

FORECE<br />

Picea excelsa<br />

T (°C)<br />

P (mm/yr)<br />

FORC LIM-E/P<br />

FORC LIM-E/P/S<br />

T (°C)<br />

T (°C)<br />

P (mm/yr)<br />

P (mm/yr)<br />

Fig. 5.4: Contour plot <strong>of</strong> Picea excelsa biomass [t/ha] as simulated by FORECE (top),<br />

FORCLIM-E/P (bottom left), and FORCLIM-E/P/S (bottom right).<br />

Compar<strong>in</strong>g <strong>the</strong> distribution <strong>of</strong> several dom<strong>in</strong>at<strong>in</strong>g tree species from Fig. 5.1 with <strong>the</strong> simulated<br />

biomass distributions, it becomes evident that extremely steep gradients are characteristic<br />

<strong>of</strong> FORECE: In this model, P. excelsa is excluded from <strong>the</strong> area where<br />

T l < 2 °C although it should approach <strong>the</strong> upper timberl<strong>in</strong>e <strong>in</strong> moist areas (Fig. 5.4).<br />

There is a similarly steep gradient <strong>of</strong> its biomass when approach<strong>in</strong>g 5 °C. In both FOR-<br />

CLIM variants, <strong>the</strong> species grows up to <strong>the</strong> alp<strong>in</strong>e timberl<strong>in</strong>e (Fig. 5.4) and decreases<br />

more smoothly towards higher temperatures, conform<strong>in</strong>g to <strong>the</strong> phytosociological expectations<br />

(Fig. 5.1). However, both FORECE and FORCLIM run <strong>in</strong>to difficulties <strong>in</strong> <strong>the</strong> area<br />

centered around 6 °C and 700 mm, where P. excelsa should dom<strong>in</strong>ate; both models exclude<br />

this species due to <strong>the</strong> occurrence <strong>of</strong> strong droughts, which may be unrealistic. It<br />

should be noted that FORECE predicts <strong>the</strong> occurrence <strong>of</strong> P. excelsa somewhat fur<strong>the</strong>r <strong>in</strong>to

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