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Keywords:

  • tidal inlet;
  • dunes;
  • sand waves;
  • water depth;
  • flow velocity;
  • grain size

[1] In the paper “Development of subaqueous barchanoid-shaped dunes due to lateral grain size variability in a tidal inlet channel of the Danish Wadden Sea” by Verner B. Ernstsen, Riko Noormets, Christian Winter, Dierk Hebbeln, Alex Bartholomä Burg W. Flemming, and Jesper Bartholdy (Journal of Geophysical Research, 110, F04S08, doi:10.1029/2004JF000180), an error appeared in Figure 3a. The corrected Figure 3 appears here.

image

Figure 3. Bed profiles along transects N2-S2 (A-E) extracted from bathymetric grids with cell sizes of 0.5 × 0.5 m from 2002 and 2003 (for locations, see Figure 2). Dune dimensions and celerities were determined from the identified (numbered from 1 to 12) large to very large dunes.

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