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Mar de nubes

De Wikipedia, la enciclopedia libre

Mar de nubes en la isla de Tenerife.

Un mar de nubes es una acumulación horizontal de estratocúmulos a baja altura (aproximadamente entre los 500 y los 1500 m), causada por vientos marítimos cargados de humedad en su sector inferior. Ello explica el fenómeno de la inversión térmica, merced al cual se registran temperaturas más altas por encima de la cota de los 1500 m que en el tramo inferior cubierto por el mar de nubes.

A cierta altura y en determinados períodos del día, el mar de nubes adquiere una tonalidad ligeramente azulada, razón de que los excursionistas menos acostumbrados lo confundan con el mar y supongan, erróneamente, que se hallan a una altitud inferior a la real.

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Esta página se editó por última vez el 11 abr 2024 a las 16:19.
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.
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