2024-03-29T01:24:34Zhttp://uvadoc.uva.es/oai/requestoai:uvadoc.uva.es:10324/406832021-06-23T10:28:30Zcom_10324_1161com_10324_931com_10324_894col_10324_1318
López Moreno, Juan Ignacio
Revuelto, Jesús
Alonso González, Esteban
Serreta, Alfredo
Serrano Cañadas, Enrique
Rico, Ibai
2020-03-23T18:06:24Z
2020-03-23T18:06:24Z
2016
Topografía y Cartografía, 2016, n. 170. p. 7-9
0212-9280
http://uvadoc.uva.es/handle/10324/40683
In this work we use a long range terrestrial laser scanner to study the evolution of the Monte Perdido Glacier, the third
largest glacier in the Pyrenees, from 2011 to the present. Scans were performed annually in late September. From 2011
to 2016, ice thinning has been obvious (-3.71 meters in average) but subjected to a marked spatial and interannual
variability. Thus, to two consecutive anomalously wet winters and cool summers (2012-13 and 2013-14), counteracted
to some degree the intense thinning that occurred during the dry and warm 2011-2012 period, but glacier thinned again
strongly in 2015, a year characterized by heavy accumulation but very warm summer conditions.
eng
info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-nd/4.0/
© 2016 Colegio Oficial de Ingeniería Geomática y Topográfica
Attribution-NonCommercial-NoDerivatives 4.0 Internacional
Geomorfología - España - Pirineos
Study of the recent evolution of Monte Perdido glacier from terrestrial laser scanner data
info:eu-repo/semantics/article