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

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H.R. Ratsimba et al. 2010. Multi-scale analysis of carbon stocks <strong>and</strong> deforestation monitoring<br />

399<br />

ecosystem <strong>and</strong> l<strong>and</strong> use conditions as well as the range of approaches to carbon credit<br />

accounting (Holmgren et al., 2008).<br />

This study is carried out in the tropical humid forest of Madagascar which is located in the<br />

eastern part of the isl<strong>and</strong>. The objective is to propose a methodology of upscaling process in<br />

deforestation <strong>and</strong> degradation assessment through satellite images (different resolutions)<br />

analysis <strong>and</strong> biomass inventory in the field. A spatial modelling approach is applied to search<br />

specific factors correlated to biomass stock, to identify vegetation indices in order to simulate<br />

the forest area across large regions, <strong>and</strong> to estimate the deforestation trend.<br />

2. Methodology<br />

2.1. Study area<br />

Madagascar should be considered among the highest conservation priorities (Myers, 1988;<br />

McNeely et al., 1990; Mittermeier et al., 1992). However, the poverty remains one of the main<br />

causes of deforestation <strong>and</strong> degradation. The average income is around $200 per year<br />

(Population Reference Bureau, 1992). Moreover, more than 70 % are from the rural regions<br />

which are facing low agricultural productivity (CIA, 2009). These situations have led to a<br />

continuous deforestation <strong>and</strong> degradation process in the whole country.<br />

The eastern part of Madagascar is characterized by a tropical humid climate with over 2000 mm<br />

mean rainfall per year <strong>and</strong> about 26°C annual mean temperature. The vegetation of this region is<br />

divided into three primary categories corresponding to elevation b<strong>and</strong>s: "lowl<strong>and</strong> rain forest" (0<br />

to 800 m), "moist montane forest" (800 to 1,300 m), <strong>and</strong> "sclerophyllous montane forest" (1,300<br />

to 2,300 m) (White, 1983). The third category is not considered in this study due to its limited<br />

repartition (the patches are to small to be evaluated in a 232 m * 232 m pixel of MODIS).<br />

There are some general trends in forest characteristics with increasing elevation: decreasing<br />

stature, fewer straight unbranched <strong>and</strong> boled trees, less stratification, more epiphytes, more<br />

bryophytes <strong>and</strong> lichens, a better developed <strong>and</strong> more diverse herb layer, <strong>and</strong> floristic changes<br />

(Lewis et al. 1996). Dense evergreen trees characterize the lowl<strong>and</strong> forest up to 800 m, with a<br />

canopy exceeding 30 m. The mid-altitude moist forest is as rich in species as the lowl<strong>and</strong> forest,<br />

but tends to have a shorter canopy of 20 to 25 m.<br />

The main threat is from subsistence agriculture through slash <strong>and</strong> burn activities (“tavy”) <strong>and</strong><br />

illegal logging which are the main causes of deforestation <strong>and</strong> degradation (Humbert, 1927;<br />

Rauh, 1979; Jolly <strong>and</strong> Jolly, 1984; Sussman et al., 1985; Jenkins, 1987).<br />

All of these aspects make REDD monitoring, reporting <strong>and</strong> verification very important for the<br />

country by creating clear <strong>and</strong> simple methods <strong>and</strong> tools to evaluate deforestation threat across a<br />

l<strong>and</strong>scape especially for policy makers <strong>and</strong> forest managers.<br />

2.2. Biomass <strong>and</strong> forest carbon accounting<br />

Biomass is defined as “organic material both above-ground <strong>and</strong> below-ground, <strong>and</strong> both living<br />

<strong>and</strong> dead, e.g., trees, crops, grass, tree litter, roots etc.” (Samalca et al., 2007). The IPCC<br />

(Intergovernmental Panel on Climate <strong>Change</strong>, 2003, 2006), has defined five different carbon<br />

pools for Greenhouse Gas (GHG) inventory : (1) living above-ground biomass (AGB), (2)<br />

living below-ground biomass (BGB), (3) dead organic matter in wood (DOM), (4) dead organic<br />

matter in litter (DOM), <strong>and</strong> (5) soil organic matter (SOM). Biomass is converted into carbon by<br />

multiplying its weight with a carbon fraction of dry matter which is usually 0.5 (IPCC, 2006).<br />

Many biomass estimation researches are focused on above-ground forest biomass (Aboal et al.,<br />

2005; Kraenzel et al., 2003; Laclau, 2003; Losi et al., 2003; Rakoto Ratsimba et al., 2010)<br />

because it represents the majority of the total biomass.<br />

This study focuses on the link between the assessment of above-ground forest biomass based on<br />

Rakoto Ratsimba et al. methods (2010) <strong>and</strong> recorded vegetation indices on satellite images.<br />

2.3. Stratification <strong>and</strong> r<strong>and</strong>omized plot based sampling<br />

Rakoto Ratsimba et al. (2010) in their study on deforestation <strong>and</strong> degradation show that the<br />

differentiation between “low degraded forest” <strong>and</strong> “degraded forest” is possible in tropical<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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