Multiple trophic levels fueled by recirculation in the Columbia River plume

Raphael M. Kudela, Alexander R. Horner-Devine, Neil S. Banas, Barbara M. Hickey, Tawnya D. Peterson, Ryan M. McCabe, Evelyn J. Lessard, Elizabeth Frame, Kenneth W. Bruland, David A. Jay, Jay O. Peterson, William T. Peterson, P. Michael Kosro, Sherry L. Palacios, Maeve C. Lohan, Edward P. Dever

Research output: Contribution to journalArticlepeer-review

35 Citations (Scopus)


Large rivers represent gateways for the transport of terrigenous and anthropogenic material to the coastal ocean. Here we document a ∼700 km 2 recirculation or bulge associated with the Columbia River plume that retains recently discharged river water sufficiently to create a regional bioreactor. Fueled by a fluvial nitrate source, this feature stimulated growth across three trophic levels and may buffer this gateway system during periods of increased warming and stratification that lead to decreased ocean productivity, potentially enhancing production at multiple trophic levels and enriching surface waters far from the river mouth.

Original languageEnglish
Article numberL18607
JournalGeophysical Research Letters
Issue number18
Publication statusPublished - 30 Sept 2010


  • trophic levels
  • Columbia River
  • recirculation
  • coastal productivity


Dive into the research topics of 'Multiple trophic levels fueled by recirculation in the Columbia River plume'. Together they form a unique fingerprint.

Cite this