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

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18 Chapter 2<br />

Swiss Plateau, which are much richer both <strong>in</strong> terms <strong>of</strong> species composition, total biomass,<br />

and soil fertility (cf. Appendix III for <strong>the</strong> location and climatic data <strong>of</strong> <strong>the</strong> sites).<br />

The additional site-specific parameters required by FORECE for <strong>the</strong> two sites are given <strong>in</strong><br />

Tab. 2.2. The simulations covered 12'000 years at each site.<br />

Emanuel et al. (1978) used spectral analysis to evaluate <strong>the</strong> behaviour <strong>of</strong> <strong>the</strong> FORET<br />

model (Shugart & West 1977). They found that up to 0.05 cycles per year account for a<br />

considerable portion <strong>of</strong> <strong>the</strong> spectral energy, correspond<strong>in</strong>g to cycles with a length <strong>of</strong> 20<br />

years. To resolve <strong>the</strong>se cycles, <strong>the</strong> sampl<strong>in</strong>g <strong>in</strong>terval must not be larger than half <strong>the</strong> cycle<br />

length. Thus <strong>the</strong> monitor<strong>in</strong>g <strong>in</strong>terval was set to 5 years <strong>in</strong> order to allow for an estimation<br />

<strong>of</strong> <strong>the</strong> spectrum <strong>of</strong> <strong>the</strong> model output.<br />

Statistical analyses <strong>of</strong> <strong>the</strong> time series data (Shumway 1988) were performed by means <strong>of</strong><br />

<strong>the</strong> SYSTAT V5.2.1 s<strong>of</strong>tware (Wilk<strong>in</strong>son et al. 1992) on Apple Mac<strong>in</strong>tosh computers.<br />

The first 1'000 years <strong>of</strong> each simulation were discarded <strong>in</strong> order to concentrate on model<br />

behaviour after <strong>the</strong> transient phase.<br />

Tab. 2.2: Additional site-specific parameters required by <strong>the</strong> FORECE model for <strong>the</strong> sites Bern and Davos<br />

(from Kienast 1987 and Kienast, pers. comm.; cf. Kienast & Kuhn 1989a,b).<br />

Parameter Davos Bern<br />

Maximum aboveground biomass [t/ha] 300 540<br />

Field capacity [cm] 27 30<br />

Wilt<strong>in</strong>g po<strong>in</strong>t [cm] 20 20<br />

Start <strong>of</strong> vegetation period [day number] 150 120<br />

End <strong>of</strong> vegetation period [day number] 227 273<br />

Frost threshold (March) [°C] 1.0 3.5<br />

Frost threshold (April) [°C] 4.0 6.5<br />

Frost threshold (May) [°C] 8.0 9.5<br />

Soil moisture <strong>in</strong>dicator value [–] 4 5<br />

Seed for random number generator -12'672 -12'672<br />

RESULTS & DISCUSSION<br />

Davos<br />

A typical part <strong>of</strong> <strong>the</strong> time series <strong>of</strong> species biomasses and tree numbers at <strong>the</strong> site Davos is<br />

shown <strong>in</strong> Fig. 2.2. From <strong>the</strong> po<strong>in</strong>t <strong>of</strong> view <strong>of</strong> biomass (Fig. 2.2 top), Norway spruce<br />

(Picea excelsa) is <strong>the</strong> dom<strong>in</strong>at<strong>in</strong>g species. Swiss stone p<strong>in</strong>e (P<strong>in</strong>us cembra) becomes im-

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