) and one intermediate polythermal glacier (Erdmannbreen). Temporal dynamics of the different suspended sediment transport systems will be inferred from the structure of statistical models which best explain the variance of proglacial suspended sediment
of polythermal-based glacier. Temporal dynamics of the different suspended sediment transport systems will be inferred from the structure of statistical models which best explain the variance of proglacial suspended sediment concentration (SSC). This constitutes