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Macro y mesoclimas del altiplano andino y desierto de Atacama: desafíos y estrategias de adaptación social ante su variabilidad

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Author(s)
Romero, Hugo
Smith, Pamela
Mendonça, Magaly
Méndez, Manuel
Keywords
Multiescalaridad
climatología
Monzón Sudamericano
Desierto de Atacama
Multiscalarity
Climatology
Tropical Monzoon
Desierto de Atacama

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URI
http://hdl.handle.net/20.500.12424/870283
Online Access
https://dialnet.unirioja.es/servlet/oaiart?codigo=5783958
Abstract
From a geographical perspective are multiscalarity analized quantitative and qualitative factors and components that give specificity to the climate of the Atacama Desert, the driest in the world, and to Andean mountains and plateaus from which depend on water sources, human settlement and economic activities, especially mining, which is the main basis for the economic growth of Chile. The South American monsoon, which brings together air masses and flows from continental inland, towards altiplanos and the Pacific coast, acts as the most important macroclimatic component, while meso-scale topoclimatic conditions, associated with exposure, altitude and topography of reliefs, determine water in the landscapes.The demand for water generated by mining boom and the adaptation strategies of indigenous communities to cope with climate change and variability provide the meaning and significance to socioclimates, which natural and socio-economic elements should be interdisciplinary and scalarly integrated.
Desde una perspectiva geográfica multiescalar son analizados cuantitativa y cualitativamente los factores y componentes que otorgan especificidad climática al desierto de Atacama, el más árido del mundo, y a las montañas y altiplanos andinos de las cuales dependen sus fuentes de agua, la ocupación humana y las actividades económicas, en especial la minería, que constituye la principal base del crecimiento económico de Chile. El monzón sudamericano, que asocia las masas y flujos de aire del interior del continente con el altiplano y la costa del océano Pacífico actúa como el componente macroclimático más relevante, mientras a mesoescala son las condiciones topoclimá-ticas, asociadas a la altura, exposición y orografía de los relieves, las que determinan la disponibilidad de agua en los paisajes. La demanda de recursos hídricos generada por el auge minero y las estrategias de adaptación de las comunidades indígenas ante las variabilidades climáticas condicionan el significado de los socioclimas, en que los elementos naturales y socioeconómicos deben ser integrados.
Date
2013
Type
text (article)
Identifier
oai:dialnet.unirioja.es:ART0001095042
https://dialnet.unirioja.es/servlet/oaiart?codigo=5783958
(Revista) ISSN 0718-3402
Copyright/License
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