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Authors
Advisor(s)
Abstract(s)
The Serra da Estrela is part of the Iberian Central Cordillera and is the highest mountain in mainland
Portugal (40◦ 20’N, 7◦ 35’W, 1993 m a.s.l.). The topoclimates are controlled by the NNE-SSW direction of
the mountain range, asymmetric exposure to the prevailing westerly air masses, high relief and irregular
morphology. Supported by a network of air temperature data loggers, the influence of the topography on
the temperature patterns has been examined. A thorough analysis of climate data from meteorological
stations, bibliographical references and the study of the terrain characteristics, including field work, remote sensing and GIS-based digital elevation model analyses, allowed the information to be synthesised
in a map of the climatopes at the scale 1:75,000. The climatopes are based on the variation of climatic
factors as a result of topography and land cover. Each climatope unit responds similarly to the forcing
induced by the atmosphere boundary layer and represents a local climate. The map includes 18 types of
climatope and contains a simple, easy-to-understand legend for the non-specialist in climatology, with
the possibility for application in land planning.
Description
Keywords
Climatopes Serra da Estrela Map Portugal
Pedagogical Context
Citation
Mora, C. (2010). A synthetic map of the climatopes of the Serra da Estrela (Portugal). Journal of Maps, 6(1), 591–608. https://doi.org/10.4113/jom.2010.1112.
Publisher
Taylor & Francis