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Susa H. Stonedahl, Judson W. Harvey and Aaron I. Packman Interactions between hyporheic flow produced by stream meanders, bars, and dunes Water Resources Research 49

Article first published online: 6 SEP 2013 | DOI: 10.1002/wrcr.20400

Key Points

  • Exchanges induced by different scales of topography are not linearly additive.
  • Dunes dominated exchange in the absence of highly sinuous meanders.
  • Interfacial flux increased with sinuosity with and without bars and dunes.

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