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The book describes an integrated theory that links estuary shape to
tidal hydraulics, tidal mixing and salt intrusion. The shape of an
alluvial estuary is characterised by exponentially varying width
and the absence of bottom slope. This topography is closely related
to tidal parameters, hydraulic parameters and parameters that
describe 1-dimensional mixing and salt intrusion. Starting from the
fundamental equations for conservation of mass and momentum,
analytical equations are derived that relate the topography to
tidal parameters (tidal excursion, phase lag, tidal damping, tidal
amplification), wave celerity, lateral and vertical mixing and salt
intrusion.
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