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Landscapes Forest and Global Change - ESA - Escola Superior ...

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N. Zurbriggen et al. 2010. Modeling feedbacks between avalanches <strong>and</strong> forests under a changing environment<br />

173<br />

snow profile, temperature). The distinct weather conditions within a few days of the event,<br />

which in reality strongly influence avalanche release probability, were not included due to the<br />

larger time scale of TreeMig (1 year steps). To be compatible with TreeMig, the avalanche<br />

module also uses one year steps. A r<strong>and</strong>om component was added to the probabilistic release<br />

module instead of explicit weather related variables, to simulate short-term (within-year)<br />

weather variability. The historical avalanche <strong>and</strong> forest data used as input was stratified into<br />

coniferous <strong>and</strong> broadleaf forest, <strong>and</strong> the GLM is run separately for each forest type.<br />

The selection criteria to include variables in the GLM were (a) significant improvement of<br />

variance explained, (b) sensitivity of at least some of the variables to climatic or l<strong>and</strong> use<br />

change, <strong>and</strong> (c) the possibility to calculate or estimate the variables from TreeMig output. To<br />

implement the equation resulting from the GLM in the avalanche module, the values for slope<br />

angle were taken from the Swiss digital elevation model (DEM) at 25m resolution (Swiss<br />

Federal Office of Topography), <strong>and</strong> maximum gap size <strong>and</strong> other forest-related variables were<br />

calculated allometrically from TreeMig output. For example, crown projection could be<br />

calculated from TreeMig output using the percent cover equations established by Lischke <strong>and</strong><br />

Zierl (2002).<br />

2.2 Mortality <strong>and</strong> regeneration modeling<br />

The increased mortality of trees st<strong>and</strong>ing in an avalanche path will be modeled based on a metamodel<br />

of RAMMS, which is currently in development. In TreeMig, different model versions<br />

will be compared, using either full mortality of all trees in the avalanche path, or partial<br />

mortality based on tree size <strong>and</strong> species. For preliminary versions of the avalanche subroutine in<br />

the forest-l<strong>and</strong>scape model, mortality will be set to one, <strong>and</strong> adapted later to include the<br />

RAMMS meta-model output.<br />

To simulate regeneration after avalanche disturbances, the dispersal, germination, establishment,<br />

<strong>and</strong> growth subroutines of TreeMig will be used (Lischke et al. 2006). Here, growth is modeled<br />

in height class increments, with a maximum possible growth rate per species, modified by<br />

environmental factors such as light, temperature, precipitation, or local disturbances. As trees<br />

are in competition for light, an increased light availability due to avalanches changes the growth<br />

potential of surviving seedlings or freshly germinated seeds.<br />

TreeMig is set up so that primary succession in the destroyed cells is given by potentially<br />

remaining seeds or seedlings, dispersal distance from mature forest, <strong>and</strong> germination <strong>and</strong><br />

growth response to environmental conditions. Seedlings that survive the avalanches will have<br />

higher growth rates due to the lower competition <strong>and</strong> higher light levels, making seedling shade<br />

tolerance <strong>and</strong> the shading function highly critical. To increase the accuracy of the seedling<br />

growth, we will partition the lowest height class (previously including all individuals 0-1.37m<br />

height) into 4 smaller classes, <strong>and</strong> improve the shading subroutine. Furthermore, the previously<br />

strict allometry between size <strong>and</strong> growth, both simulated in units of height classes, will be<br />

improved by allowing more variability between size <strong>and</strong> growth. This is especially important at<br />

treelines, where individuals are often found to be relatively old, but short, with a relatively high<br />

stem diameter.<br />

2.3 Merging of model components<br />

The four components of avalanche release <strong>and</strong> flow inside <strong>and</strong> outside of forested areas will be<br />

implemented in the forest l<strong>and</strong>scape model TreeMig, <strong>and</strong> analyzed for sensitivity, scaling<br />

effects, <strong>and</strong> model uncertainties. To implement the avalanche module in TreeMig, both the<br />

avalanche submodel <strong>and</strong> the growth <strong>and</strong> regeneration subroutines require careful calibration.<br />

<strong>Forest</strong> <strong>L<strong>and</strong>scapes</strong> <strong>and</strong> <strong>Global</strong> <strong>Change</strong>-New Frontiers in Management, Conservation <strong>and</strong> Restoration. Proceedings of the IUFRO L<strong>and</strong>scape Ecology<br />

Working Group International Conference, September 21-27, 2010, Bragança, Portugal. J.C. Azevedo, M. Feliciano, J. Castro & M.A. Pinto (eds.)<br />

2010, Instituto Politécnico de Bragança, Bragança, Portugal.

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