Sistema de observación meteorológica

Posted in Climate

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Más de 20 años realizando observaciones meteorológicas en el Parque Nacional

Desde el año 1998 se llevan a cabo, de forma continuada, observaciones de diversos parámetros meteorológicos en el valle de El Paular, Parque Nacional de la Sierra de Guadarrama. Esto supuso un hito en la observación meteorológica en alta montaña y desde entonces existe un compromiso firme del Parque Nacional Sierra de Guadarrama para mantener unas observaciones pioneras y fundamentales para un seguimiento adecuado del clima de este territorio y, por extensión, de todo el planeta.

Los objetivos prinicipales de este sistema de observación son:

  • hacer un seguimiento riguroso del clima;
  • conocer las condiciones meteorológicas reinantes;
  • promover la realización de estudios científicos relacionados con su gestión y conservación.

En todos esto años han participado, y siguen participando, numerosas personas que garantizan con su esfuerzo y profesionalidad la continuidad y calidad de las medidas obtenidas, personal del Parque o contratadas en el marco de la gestión del Parque Nacional Sierra de Guadarrama.

Estado del tiempo

Posted in Climate

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The Sierra de Guadarrama Climate

Posted in Climate

Ventisca en el Puerto de CotosThe Sierra de Guadarrama, along with the Gredos and Ayllón Sierras, makes up the Sistema Central (the Central System). This chain of mountains runs basically in West-East direction and splits the meseta in two subplateaux having different continental mediterranean climates. The orography of the Central System has a direct influence on the Iberian Peninsula climate; the Northern area has a temperate climate, with dry and warm summers (Csb according to Köppen climate classification) and the Southern region has dry and hot summers (Csa). Csb climate is the one dominating in the Sierra de Guadarrama.

This continental mediterranean climate, typical of the peninsular interior, overlaps in the Sierra de Guadarrama with the mountain climate, with very cold winters and dry chilly summers. As the height increases, there is a precipitation and temperature gradient across the Sierra, so precipitation is more copious and, generally, in the form of snow. On the other hand, the temperature varies inversely to the height.

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