Morphology of estuarine bedforms, Weser Estuary, Germany. Issue 1 (13th October 2021)

• Record Type: Journal Article
• Authors: Lefebvre, Alice; Herrling, Gerald; Becker, Marius; Zorndt, Anna; Krämer, Knut; Winter, Christian
• Is Part Of: Earth surface processes and landforms. Volume 47:Issue 1(2022)
• Page Start: 242
• Page End: 256
• Publication Date: 2021-10-13
• Subjects: bedform shape -- bedform size -- data analysis -- dunes -- hydraulic roughness; Geomorphology -- Periodicals; 551.4
• DOI: 10.1002/esp.5243
• Languages: English
• ISSNs: 0197-9337

Abstract

Abstract: Large bedforms (dunes) are present in many shallow‐water environments. Knowledge of their dimensions and dynamics is required for river and coastal management. In tidal rivers and estuaries, the interaction among hydrodynamics (which results from the action of river and tidal flows), sediment transport and bedform shape and size is complex. In the present study, the distribution and morphology of bedforms in the Weser Estuary, Germany, were investigated. Bedforms were identified in bathymetric data of monthly multibeam echosounder surveys along the navigation channel during the years 2009 to 2013. Their size and shape were characterized. Bedforms were present along most of the channel, except at the position of the estuarine turbidity maximum and where dredging is carried out. Average bedform length varied between 20 and 60 m and bedform height between 0.3 and 1.6 m. Bedform asymmetry varied spatially and temporally along the estuary. In times of high river discharge, bedforms were generally more ebb‐asymmetric than in times of low discharge. The bedforms were predominantly two‐dimensional low‐angle dunes with their steepest slope situated near the bedform crest. A significant proportion of bedforms possessed a steep face (portion of the lee side steeper than 15°). This implies that they are likely to create flow separation and a turbulent wake, with a strong potential to induce high bedform roughness. However, important variations in steep face area density were noted, both spatially along the estuary and temporally as a function of the tidal phase (ebb or flood) and the seasonal variation in river discharge. The results have wide implications in terms of understanding and modelling hydrodynamics and sediment transport in estuaries. Abstract : Bedforms are present along most of the Weser Estuary channel and their properties vary spatially and temporally. Bedforms are predominantly two‐dimensional low‐angle dunes with their steepest slope situated near the bedform crest. The steep face (portion of the lee side steeper than 15°) area density is used to assess over which bedforms flow separation and turbulent wake are likely to happen.