Low flows in alpine systems: New insights from a year without snow in the Cascade Mountains of Oregon, USA
Abstract
We examine stream flow recession in the Cascade Mountains of Oregon. A new method to compute the recession parameters is presented. The characteristic drainage timescales of the young volcanic systems were found to be 5x longer than the older watersheds. We demonstrate how the “maturity” of the landscape and its river network control such different hydrological behavior. Show more
Publication status
unpublishedPublisher
ETH ZurichEvent
Organisational unit
03465 - Löw, Simon (emeritus) / Löw, Simon (emeritus)
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