Analytical approach for determining the mean water level profile in an estuary with substantial fresh water discharge

The mean water level in estuaries rises in the landward direction due to a combination of the density gradient, the tidal asymmetry, and the backwater effect. This phenomenon is more prominent under an increase of the fresh water discharge, which strongly intensifies both the tidal asymmetry and the...

Full description

Bibliographic Details
Main Authors: H. Cai, H. H. G. Savenije, C. Jiang, L. Zhao, Q. Yang
Format: Article
Language:English
Published: Copernicus Publications 2016-03-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/20/1177/2016/hess-20-1177-2016.pdf