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11 th International Symposium for GIS and Computer Cartography for Coastal Zones ManagementThe potential sea level rise may disrupt physical and biological systems, but also affect society in a comprehensiveway, with possible consequences for our natural heritage and production systems. In the impact analysis of climatechange it is important to consider integrating both environmental and social dimensions. This was performedby two indices: IREC - index of ecological relevance. It is calculated as a sum of twelve standardized variables. Ten variablescorrespond to the potential wealth of species and number of threatened species (five fauna groupswere observed: mollusks, amphibians, reptiles, birds and mammals). The two remaining variables arenumber of vegetation formation and number of vegetation threatened formations. (Brazeiro et al., 2009) ID - index population. Population density of the coastal towns was taken from the 2004 census data andcategorized into five classes through natural intervals.ConclusionsApproximately 30% of coastal squares have high or very high vulnerability value to sea level rise. A generalanalysis shows that the spatial variability of CVI is mainly determined by the categories of erosion, slope and geomorphologiclandforms. Meanwhile, variables like sea level rise, tidal range and wave height have less spatial variability.When ecological or social variables are included, we are able to see another picture of the situation. This kindof “GIS-game” builds up a helpful and always more wide-ranging tool to decision making.ReferencesAlvez, M. (2011), Mapa de vulnerabilidad a la erosión costera de la costa atlántica uruguaya. Degree thesis Universidad de laRepública, Uruguay, 88p.Brazeiro, A., C. Toranza, and L. Bartesaghi (2009), Biodiversidad Costera Resultado 7, Proyecto URU 06/016: 2.3.3 ConvenioEcoPlata – Udelar/Facultad de Ciencias. Uruguay.Gornitz, V.M., R.C. Daniels, T.W. White, and K.R. Birdwell (1994), “The development of a coastal risk assessment database:Vulnerability to sea-level rise in the U.S. southeast”. Journal of Coastal Research, Special Issue 12: 327–338.Goso, C. and V. Mesa (2009), Mapas de riesgo geológico a la escala macro de la costa uruguaya y para los sitios piloto frentesalino– franja costera y Laguna de Rocha. Informe Nº II: Resultados 3, 6 y 8 del Convenio FCien – Proyecto URU/07/G32,Montevideo.IPCC (2007), Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth AssessmentReport of the Intergovernmental Panel on Climate Change. S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K.B.Averyt, M. Tignor and H.L. Miller (eds.). Cambridge University Press, Cambridge, United Kingdom. 996 pp. Retrieved fromfrom:http://www.ipcc.ch/publications_and_data/publications_ipcc_fourth_assessment_report_wg1_report_the_physical_science_basis.htmKokot, R., J. Codignotto, and M. Elissondo (2004), “Vulnerabilidad al ascenso del nivel del mar en la costa de la provincia deRío Negro”. Revista de la Asociación Geológica Argentina, 59 (3):477–487.López-Laborde J., A. Perdomo, and M. Gómez-Erache (eds.) (2000), Diagnóstico Ambiental y Socio-Demográfico de la ZonaCostera Uruguaya del Río de la Plata, EcoPlata, Montevideo, Uruguay, 991p.RENARE – MGAP Dirección Nacional de Recursos Renovables, Ministerio de Ganadería Agricultura y Pesca (2003), ModeloDigital de Terreno de la República Oriental del Uruguay. Montevideo, Uruguay: Author.Thieler, E.R., S.J. Williams, and R. Beavers (2001), Relative Coastal Vulnerability Assessment of National Park Units to Sea-Level Rise. Fact Sheet 095-02. USGS.44

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