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

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Behaviour <strong>of</strong> FORCLIM along a transect <strong>in</strong> <strong>the</strong> European Alps 115<br />

There are two fundamental questions to be addressed with<strong>in</strong> this context:<br />

1) How close to <strong>the</strong> “true” equilibrium state are <strong>the</strong> estimates as a function <strong>of</strong> n<br />

and ∆t? In addition to <strong>the</strong>oretical reason<strong>in</strong>g, simulation experiments can yield<br />

quantitative <strong>in</strong>formation on <strong>the</strong> precision <strong>of</strong> such estimates.<br />

2) How similar to each o<strong>the</strong>r are two estimates <strong>of</strong> <strong>the</strong> same steady state, us<strong>in</strong>g a<br />

given n and ∆t? This question is especially important if two model variants are<br />

to be compared, e.g. for assess<strong>in</strong>g <strong>the</strong> effect <strong>of</strong> climatic change on species<br />

composition. Moreover, is it possible to develop a threshold for significant<br />

differences between steady states for a given n and ∆t?<br />

4.4.1 Material & methods<br />

To answer <strong>the</strong> above two questions, two sets <strong>of</strong> simulation experiments were conducted<br />

with <strong>the</strong> FORCLIM-E/P model. From <strong>the</strong> analysis <strong>in</strong> section 2.2.1, it can be hypo<strong>the</strong>sized<br />

that temporal autocorrelation is important at lags up to more than 100 years, and <strong>the</strong> data<br />

from section 2.2.2 suggest that <strong>the</strong> sample size should be larger than 100. Thus, to answer<br />

question 1, a factorial design was used with n = 50, 100, 200, 400, 1000, and<br />

∆t = 100, 150 years. This yielded a total <strong>of</strong> 10 experimental setups. For each setup, 20<br />

simulation runs were performed, and a steady state was estimated from each run. The<br />

first 1000 years <strong>of</strong> each simulation were discarded (transient behaviour, cf. chapter 4).<br />

The “true” equilibrium was assumed to be <strong>the</strong> average <strong>of</strong> <strong>the</strong> 20 steady states estimated<br />

with n = 1000 and ∆t = 150, thus correspond<strong>in</strong>g to 20'000 po<strong>in</strong>ts. The percentage similarity<br />

coefficient (PS) <strong>in</strong>troduced <strong>in</strong> Eq. 2.3 was used for compar<strong>in</strong>g <strong>the</strong> steady states,<br />

and simulations were conducted for <strong>the</strong> site Bern (cf. Appendix III).<br />

From <strong>the</strong>se results, <strong>the</strong> comb<strong>in</strong>ation <strong>of</strong> n = 200 and ∆t = 150 years was chosen for fur<strong>the</strong>r<br />

study, i.e. to answer question 2. It may be hypo<strong>the</strong>sized that it is easier – both <strong>in</strong> a<br />

forest gap model and <strong>in</strong> reality – to estimate <strong>the</strong> composition <strong>of</strong> a species-poor forest with<br />

one dom<strong>in</strong>at<strong>in</strong>g species than that <strong>of</strong> a diverse forest with many co-dom<strong>in</strong>at<strong>in</strong>g species.<br />

Moreover, <strong>the</strong> abundance <strong>of</strong> a species that is always present on a patch but has low biomass<br />

is easier to estimate than that <strong>of</strong> a species with episodic occurrence, but that atta<strong>in</strong>s<br />

large biomass when it is present. Thus, <strong>the</strong> PS between <strong>in</strong>dependent estimates <strong>of</strong> <strong>the</strong><br />

same steady state at a given site should depend on <strong>the</strong> number <strong>of</strong> species and <strong>the</strong>ir roles at<br />

that site (cf. Shugart 1984). To test this hypo<strong>the</strong>sis, 400 steady states were estimated at

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