Spatial characterization of glacial and periglacial landforms in the highlands of Sierra Nevada (Spain)

P Palma; M Oliva; C García-Hernández; A Gómez Ortiz; J Ruiz-Fernández; F Salvador-Franch; M Catarineu

doi:10.1016/j.scitotenv.2017.01.196

Spatial characterization of glacial and periglacial landforms in the highlands of Sierra Nevada (Spain)

Sci Total Environ. 2017 Apr 15:584-585:1256-1267. doi: 10.1016/j.scitotenv.2017.01.196. Epub 2017 Feb 8.

Authors

P Palma¹, M Oliva², C García-Hernández³, A Gómez Ortiz⁴, J Ruiz-Fernández³, F Salvador-Franch⁴, M Catarineu⁴

Affiliations

¹ Centre for Geographical Studies-IGOT, Universidade de Lisboa, Lisbon, Portugal. Electronic address: p.palma@campus.ul.pt.
² Centre for Geographical Studies-IGOT, Universidade de Lisboa, Lisbon, Portugal.
³ Department of Geography, University of Oviedo, Oviedo, Spain.
⁴ Department of Geography, University of Barcelona, Barcelona, Spain.

PMID: 28189311
DOI: 10.1016/j.scitotenv.2017.01.196

Abstract

Sierra Nevada constitutes the southernmost and highest massif in the Iberian Peninsula, with elevations exceeding 3000m. Two large glacial advances were recorded during the Last Glaciation and several minor advances occurred until the Early Holocene. Since then, periglacial activity has prevailed above 2500m. Here, we present a new and more accurate geomorphological map of the highlands of Sierra Nevada, integrating in a GIS environment i) high resolution satellite imagery, ii) topographic data, and iii) field observations. This approach has allowed a better characterization of the spatial extent of cold-climate morphogenic processes and associated landforms formed during the Last Glaciation and subsequent deglaciation. Despite its extension and high altitude, the steep relief of Sierra Nevada and its southern location conditioned a significantly lower glaciated surface (104.6km²) with respect to other Iberian massifs. We have also inferred the paleoclimatic conditions of the study area through the calculation of Equilibrium Line Altitudes (ELAs). The distribution of the lowest moraines suggests an ELA for the maximum glacial extent at 2525m in the northern slope and 2650m in the southern side, increasing towards the east. Local ELA differences are related to: (i) the influence of the warmer Mediterranean Sea in contrast to the cooler Atlantic Ocean, (ii) the climate with more continental characteristics on the northern slope, and (iii) the microscale control of the local topography. Mean annual air temperatures in the ice-free summit plateaus were between -4/-6°C during the maximum local glacial extent, determining permafrost conditions with intense periglacial dynamics. Rock glaciers and protalus lobes developed until 2500m, the lowest boundary for permafrost regime. The distribution of other glacial and periglacial landforms within the limits of the maximum ice extent provides evidence to better understand the extent of subsequent glacial stages and post-glacial landscape evolution in Sierra Nevada.

Keywords: Equilibrium Line Altitude; Geomorphological map; Glacial and periglacial landforms; Glacier reconstruction; Last Glaciation; Paleoclimate; Sierra Nevada.