The relatively warm climate conditions prevailing today in the Mediterranean region limit
cold geomorphological processes only to the highest mountain environments. However …

In GPR profiles, ice is usually imaged as a mostly electromagnetic transparent facies.
However, diffraction events, as well as internal layering, can be also observed. In some …

Permafrost in high alpine catchments is expected to disappear in future warmer climates, but
the hydrological impact of such changes is poorly understood. This paper investigates the …

It is well known that small glaciers of mid latitudes and especially those located at low
altitude respond suddenly to climate changes both on local and global scale. For this reason …

Among the different elements of the mountain cryosphere, ice caves still represent the lesser
known part of it. Here we present a seven-year-long record of air and rock temperature in a …

High altitude karstic environments often preserve permanent ice deposits within caves,
representing the lesser-known portion of the cryosphere. Despite being not so widespread …

Data from geocryological studies of soil and rock massifs in permafrost zone are very
important as a basis for predicting possible negative consequences associated with climate …

Ground penetrating radar (GPR) has proven to be a very effective method for examining ice
thickness. However, two preconditions must be met for this approach to be useful; the round …

Dolines and shafts are common geomorphologies in karst landscapes. When affected also
by glacial processes, they are considered an example of glaciokarst landform. In high alpine …

We reconstruct englacial and subglacial drainage at Skálafellsjökull, Iceland, using ground
penetrating radar (GPR) common offset surveys, borehole studies and Glacsweb probe …