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This report provides a detailed outline of a newly enhanced estuary database which comprises a wide array of both qualitative descriptive parameters and “generalised” quantitative physical estuarine p...
In the period from 26th July to 26th August 2004, the Yellow River Conservancy Commission conducted a field experiment of warping on the floodplain of Libotan in the Middle Yellow River.Six experiment...
Understanding coastal processes is increasingly important because the ma jority of the world’s shoreline are eroding. Global warming and storm surges due to extreme weather conditions further threat h...
Within the framework of Delft Cluster Project “Ecomorphology of Estuaries and Coast”, a model for the long-term morphological development of the Feiyun Estuary in Zhejiang, China, has been set up. The...
The Naruse River mouth showed stable topography at least for these 46 years. However, sediment deposit occurred in July 2002, which caused difficulty in ship operation going in and out of a port loca...
Nodal tide variation causes a periodic change of the mean tidal range with a period of 18.6 years and amplitude of about 4%. As the cross-sectional area of the channels in estuaries is related to the ...
A mathematical model for calculating river mouth width is introduced, by considering sediment intrusion by waves, as well as sediment flushing by river and tidal discharge. Behavior of an analytical s...
The Netherlands are situated on the delta of three of Europe's biggest rivers: the Rhine, the Meuse and the Scheldt, at the border of a shallow regional sea : the North Sea (see Fig. 1). Without dikes...

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