5.6. DIWA-webinaari

Henri Heiskanen, Aalto University, henri.heiskanen@aalto.fi Streamflow, or river discharge (Q), is a core variable in hydrology. It describes the volume of water passing a given river cross-section per unit time and is required for watershed water balance calculations as well as for practical water resources management, including flow regulation and

Eeva Järvi-Laturi, University of Oulu. eeva.jarvi-laturi@oulu.fi This summer, I found myself knee-deep in a peatland—both literally (almost lost a boot!) and figuratively. As part of my PhD, I spent the short but intense growing season mostly out in the field, chasing data across gradients, depths, and disciplines. It was a