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Article
K. C. Wong, AuteurThe buoyant discharge from Delaware Bay forms two separate branches of residual outflow near the bay mouth, one along each shore. Upon exiting the bay, the branch along the Delaware shore turns right to form the southward flowing Delaware coasta[...]
Article
C. D. Janzen, Auteur ; K. C. Wong, AuteurThe low-frequency transport processes in a small, shallow coastal lagoon (Indian River Bay, Delaware) are examined based on a set of data derived from tide gauges, near-bottom current meter measurements, and drifter releases. The subtidal sea-le[...]
