The University of Sheffield
Department of Geography

Glacier hydrology and hydrometeorology

Rhodamine WT

A detailed, system-scale characterisation of glacier hydrology is essential in order to understand the fluxes of nutrients from snow and ice reservoirs and their interaction with ice-marginal environments. Further, glacier hydrology tells us how ice mass dynamics respond to melt and thus climate change. Recent work suggests that high latitude glaciers do not conform to expectation, largely because these expectations were developed from the study of temperate glaciers at lower latitudes. Thus new models are required that better explain the passage of surface-derived meltwaters through such glaciers and particular attention should be given to their role in the decoupling of the glacier from its bed.

Aerial shot of one of our dye pulses upon Midtre Lovenbreen, Svalbard (courtesy of High Spy). Single dye injections can emerge from multiple subglacial outflows, suggesting that conventional models of glacial drainage structure may not apply here.

Relevant papers