Researchers review hydrologic, geomorphic, ecologic, and social conditions in the Willamette River basin through time—including pre-settlement, river development, and contemporary periods—and offer a future vision for consideration.
Researchers found data from wind tunnel experiments indicate there is a spatial lag from the canopy leading edge to a downwind location where sediment deposition first occurs.
This article highlights a few of the programs and tools that Oregon Sea Grant has developed and challenges readers to join the effort to increase resilience throughout the nation.