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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
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Volume 6, issue 3 | Copyright
Earth Surf. Dynam., 6, 763-778, 2018
https://doi.org/10.5194/esurf-6-763-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 11 Sep 2018

Research article | 11 Sep 2018

Morphology of bar-built estuaries: empirical relation between planform shape and depth distribution

Jasper R. F. W. Leuven, Sanja Selaković, and Maarten G. Kleinhans Jasper R. F. W. Leuven et al.
  • Faculty of Geosciences, Utrecht University, Princetonlaan 8A, 3584 CB, Utrecht, the Netherlands

Abstract. Fluvial–tidal transitions in estuaries are used as major shipping fairways and are characterised by complex bar and channel patterns with a large biodiversity. Habitat suitability assessment and the study of interactions between morphology and ecology therefore require bathymetric data. While imagery offers data of planform estuary dimensions, only for a few natural estuaries are bathymetries available. Here we study the empirical relation between along-channel planform geometry, obtained as the outline from imagery, and hypsometry, which characterises the distribution of along-channel and cross-channel bed levels. We fitted the original function of Strahler (1952) to bathymetric data along four natural estuaries. Comparison to planform estuary shape shows that hypsometry is concave at narrow sections with large channels, while complex bar morphology results in more convex hypsometry. We found an empirical relation between the hypsometric function shape and the degree to which the estuary width deviates from an ideal convergent estuary, which is calculated from river width and mouth width. This implies that the occurring bed-level distributions depend on inherited Holocene topography and lithology. Our new empirical function predicts hypsometry and along-channel variation in intertidal and subtidal width. A combination with the tidal amplitude allows for an estimate of inundation duration. The validation of the results on available bathymetry shows that predictions of intertidal and subtidal area are accurate within a factor of 2 for estuaries of different size and character. Locations with major human influence deviate from the general trends because dredging, dumping, land reclamation and other engineering measures cause local deviations from the expected bed-level distributions. The bathymetry predictor can be used to characterise and predict estuarine subtidal and intertidal morphology in data-poor environments.

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This paper reports the along-channel variability in occurring bed levels as described by hypsometry in natural estuaries. We found a novel relation between the estuary planform shape and the hypsometric function shape, which implies that it is possible to characterise and predict subwater estuarine morphology and bed levels in data-poor environments.
This paper reports the along-channel variability in occurring bed levels as described by...
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