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

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R.A. Diaz-Varela et al. 2010. Quantitative assessment of temporal dynamics in altitudinal-driven ecotones<br />

353<br />

of herbaceous formations, dwarf scrubs <strong>and</strong> thickets take place. Woodl<strong>and</strong>s with variable<br />

density of scattered <strong>and</strong> often stunted individuals of pine (Pinus sylvestris, P. mugo), spruce<br />

(Picea abies) <strong>and</strong> larch (Larix decidua) occur between this treeless area <strong>and</strong> dense forest<br />

formations. These species also dominate the high altitude forests, while the lower parts are<br />

covered by different tree formations dominated by deciduous broadleaved species. Hay<br />

meadows are the most common agricultural l<strong>and</strong>, occupying only a small surface at valley<br />

bottoms, while arable l<strong>and</strong> is virtually absent in the area.<br />

2. Methodology<br />

We started with the stereoscopic analysis <strong>and</strong> visual interpretation of aerial photos from 1954<br />

<strong>and</strong> 2003 to generate a raster map with the distribution of close forest, scattered trees <strong>and</strong> alpine<br />

tundra for each of the dates. We then used a spatial overlay technique to analyse the temporal<br />

change of the three classes. The overlay outputs were arranged in a 44 contingency matrix<br />

using as input the 1954 (columns) <strong>and</strong> 2003 (rows) raster maps, <strong>and</strong> considering 4 classes,<br />

namely: “Dense forest”, “Scattered trees”, “Tundra” <strong>and</strong> “Other”. Overall Kappa <strong>and</strong> Kappa<br />

indices for each l<strong>and</strong> cover class (Cohen 1960) were used as estimators of the rate of change, as<br />

suggested in other studies (Calvo-Iglesias et al. 2006).<br />

We then applied an algorithm developed by Diaz Varela et al. (2010) to identify the uppermost<br />

pixel of targeted ecotones for each of these maps. The method used to delineate forest line, tree<br />

line <strong>and</strong> tundra line ecotones follows the general definition of tree line by Körner (1999) <strong>and</strong><br />

aims at performing the automatic discrimination of elements (outpost) with an uppermost<br />

extreme position on a certain slope. Outposts corresponded to the uppermost pixels of each of<br />

the three l<strong>and</strong> cover classes <strong>and</strong> they were used to represent <strong>and</strong> map the ecotones. That is, for<br />

the l<strong>and</strong> cover class “forest”, outposts define the forest line; the “dense forest” plus “scattered<br />

trees” class outposts define the tree line <strong>and</strong> the “tundra” class outposts define the tundra line.<br />

An outpost is herein defined according to this example regarding trees: an operator in the field<br />

will define a tree as belonging to the tree line if he encounters no other tree while walking<br />

upward in the direction of maximum slope for as long as possible (i.e. until a summit is reached).<br />

Therefore, the trajectory from a given point will move upward following a maximum slope path<br />

until it encounters another element of the same class or finishes at a summit large enough to<br />

define a slope or series of slopes with similar exposure at a certain scale (cf. fig 2). Extending<br />

this concept from single trees to a the maps of forests, trees <strong>and</strong> tundra, the algorithm was<br />

implemented in ITT-IDLTM V. 6.3 to label the cells of a binary l<strong>and</strong> cover map (in this case<br />

tree – no tree) as belonging to the ecotone or not (see Diaz-Varela et al. 2010 for a more<br />

thorough description of the method).<br />

The temporal evolution of the different ecotones was analysed by extending the algorithm to a<br />

diachronic map. For the identification of ecotone altitude advances we ran upward flow paths<br />

from any upslope outpost pixel for 1954 until a 2003 upslope outpost pixel or a summit was<br />

reached. Altitude retreats were computed with the same scheme but using 2003 <strong>and</strong> 1954<br />

ecotone pixels as starting <strong>and</strong> end points, respectively. Therefore, where the ecotone location in<br />

1954 appeared in a higher position than in 2003 along a given maximum slope line, it was<br />

possible to trace <strong>and</strong> quantify the retreat or negative altitudinal shift.<br />

To characterise morphologically the spatial pattern of the outposts for the three ecotones in the<br />

period of reference <strong>and</strong> to assess changes in vegetation dispersion strategies, we used the<br />

GUIDOS software (Graphical User Interface for the Description of image Objects <strong>and</strong> their<br />

Shapes). This software was recently developed for morphological spatial pattern analysis<br />

(MSPA) of forest functional connectivity in the context of biodiversity studies (Vogt et al. 2008,<br />

Vogt et al., 2009). The output of the MSPA is a raster layer where patch cells are assigned to<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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