The aims of this review are to:(a) describe and interpret structures in valley glaciers in
relation to strain history; and (b) to explore how these structures inform our understanding of …

Microbial communities and nutrient dynamics in glaciers and ice sheets continuously
change as the hydrological conditions within and on the ice change. Glaciers and ice sheets …

Directly observing glacial drainage systems (englacial and subglacial) is challenging. The
distribution, morphology and internal structure of eskers can provide valuable information …

Englacial conduits act as water pathways to feed surface meltwater into the subglacial
drainage system. A change of meltwater into the subglacial drainage system can alter the …

The widely used tool, ground penetrating radar (GPR), has proven to be an excellent
research method for glaciological studies. The total ice thickness and englacial structures …

Hydrological systems of glaciers have a direct impact on the glacier dynamics. Since the
1950s, geophysical studies have provided insights into these hydrological systems …

Understanding glacier drainage system behaviour and its response to increased meltwater
production faces several challenges in the High Arctic because many glaciers are …

This chapter is dedicated to the assessment of the applicability of the existing models toward
the study of the landscape evolution in the three poles, that is, the Arctic, the Antarctic, and …

Meltwater routing through ice masses exerts a fundamental control over glacier dynamics
and mass balance, and proglacial hydrology. However, despite recent advances in mapping …

Surface nuclear magnetic resonance (SNMR) is a geophysical technique that is directly
sensitive to liquid water. In this study, we evaluate the feasibility of SNMR for detecting and …