First evidence of rock wall permafrost in the Pyrenees (Vignemale peak, 3,298 m a.s.l., 42°46′16″N/0°08′33″W)

Article

Abstract: Permafrost is a relevant component of the Pyrenean high mountains, triggering a wide range of geomor

Palabras claves:

climate warming, Pyrenees, rock surface temperature, rock wall permafrost, temperature modeling, Vignemale peak

Autores:

Alonso-González E., Enrique Serrano, Gómez-Lende M., Hughes-Allen L., López-Moreno J.I., Magnin F., Revuelto J., Rico I.

Fuentes:

scopus