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This paper analyses the topographic context of the remaining glaciated areas in the Maladeta
Massif (Central Spanish Pyrenees). These ice-covered surfaces have been incorporated into a
geographic information system (GIS) in an attempt at correlating the presence of ice with a
range of topographic variables obtained from a digital elevation model. The use of generalized
additive models and binary regression tree models enabled us (i) to quantify the spatial
variability in the distribution of glaciers attributable to characteristics of the local terrain,
(ii) to investigate the interaction between the variables that account for the ice cover distribution
and (iii) to map the probability of glacier development. Our results show that
although the development of glaciers depends on regional climate conditions, the topographic
context is of paramount importance in determining the location, extent, shape and recent
evolution of each glacial body. Thus, the joint effect of altitude, exposure to incoming solar
radiation, slope and mean curvature is able to explain more than 70 per cent of the observed
variance. | |
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