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

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J. Russell et al. 2010. Developing models <strong>and</strong> processes to aid decision support for integrated l<strong>and</strong> management<br />

533<br />

ILM <strong>and</strong> CEA. The plan would demonstrate that it was feasible to produce an ILM/CEA<br />

structure, models could be developed or adapted, <strong>and</strong> outcomes could be tested over time.<br />

2. Methodology<br />

In 1995, Millar Western developed permanent vegetation sample plots that focused on tree<br />

growth, as well as free-to-maneuver flying space, bat crevices, tree lichen cover <strong>and</strong> downed<br />

woody debris. Additional research included creel censuses, thinning trials to evaluate tree<br />

growth <strong>and</strong> habitat use, tree retention in clearcut st<strong>and</strong>s, animal surveys <strong>and</strong> habitat supply<br />

model verification. In 1997, expert panels were assembled to develop models for: l<strong>and</strong>scape<br />

projection under various climate change scenarios; coarse <strong>and</strong> fine filter habitat supply <strong>and</strong>;<br />

surface water quantity <strong>and</strong> quality. Research outcomes <strong>and</strong> the mechanisms developed would be<br />

incorporated into a timber supply model as constraints against the allowable cut.<br />

2.1 L<strong>and</strong>scape Projection<br />

The L<strong>and</strong>scape group used the Special Report on Emissions Scenario A1 (IPCC 2001) to predict<br />

impacts on the forest of climate change, namely a doubling in atmospheric CO 2 concentrations,<br />

<strong>and</strong> an increase of 7ºC in temperature <strong>and</strong> 8% in precipitation between 1999 <strong>and</strong> 2100 (Millar<br />

Western <strong>Forest</strong> Products 2007). To project climate conditions, the CCSR-NIES <strong>Global</strong><br />

Circulation Model (Ozawa et al. 2001) was selected. To downscale climate data, local weather<br />

was adjusted with global circulation model data. The FORECAST model (Kimmins et al. 1999)<br />

was used to predict forest growth <strong>and</strong> the Athabascan Plains L<strong>and</strong>scape model was used to<br />

predict forest succession changes (Yamasaki et al. 2008). Nine scenarios were tested <strong>and</strong><br />

biodiversity <strong>and</strong> productivity were evaluated within these l<strong>and</strong>scape projections (Yamasaki et al.<br />

2008). The study area sits at the northern limit of the Aspen Parkl<strong>and</strong> ecoregion <strong>and</strong> research<br />

has suggested that climate change may result in the conversion of forested l<strong>and</strong> to aspen<br />

parkl<strong>and</strong> (Hogg <strong>and</strong> Hurdle 1995). Therefore this analysis included prediction of how much<br />

forested l<strong>and</strong> would shift to aspen parkl<strong>and</strong> under climate change Scenario A1 (IPCC 2001).<br />

Daily fire weather indices were calculated once weather streams under historical <strong>and</strong> climate<br />

change conditions were obtained. The Fire Behavior Prediction System (<strong>Forest</strong>ry Canada Fire<br />

Danger Group 1992) was used to derive daily values for the Fine Fuel Moisture Code, Build Up<br />

Index <strong>and</strong> Fire Weather Index for the period 1 January 1961 to 31 December 1990 <strong>and</strong> the<br />

corresponding 30-year period under climate change. This fire record, which corresponds to the<br />

30-year baseline most commonly used in climate research, serves as the basis for fire modelling<br />

with the Athabascan Plains L<strong>and</strong>scape Model. To simulate 200 years of fires, the model cycles<br />

through this 30-year record almost seven cycles. Fire duration, extent, frequency <strong>and</strong> seasonality<br />

were all statistically modelled as dependents of the Fire Behavior Prediction indices above <strong>and</strong><br />

annual, seasonal <strong>and</strong> daily measures of temperature, precipitation <strong>and</strong> wind. A link detected<br />

among fire occurrence, weather <strong>and</strong> human population was also included in the analysis.<br />

As an example of a dominant non-forestry related human disturbance in the FM area, patterns of<br />

oil <strong>and</strong> gas development were analyzed <strong>and</strong> future developments were simulated. The number of<br />

current wells was determined from the forest inventory. It was also possible to generate a time<br />

series of number of new well sites annually, <strong>and</strong> the area each represents. This was also<br />

completed for pipelines <strong>and</strong> seismic lines that are projected to being developed in the FM area.<br />

2.2 Habitat Supply<br />

Coarse filter analysis was divided into two areas within the Biodiversity Assessment Project<br />

(BAP): ecosystem diversity <strong>and</strong> l<strong>and</strong>scape configuration (Van Damme et al. 2003). Ecosystem<br />

diversity analysis assumes that silvicultural practices will modify the distribution of ecosystems<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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