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It is the task of the engineer, as of any other professional
person, to do everything that is reasonably possible to analyse the
difficulties with which his or her client is confronted, and on
this basis to design solutions and implement these in practice. The
distributed hydrological model is, correspondingly, the means for
doing everything that is reasonably possible - of mobilising as
much data and testing it with as much knowledge as is economically
feasible - for the purpose of analysing problems and of designing
and implementing remedial measures in the case of difficulties
arising within the hydrological cycle. Thus the aim of distributed
hydrologic modelling is to make the fullest use of cartographic
data, of geological data, of satellite data, of stream discharge
measurements, of borehole data, of observations of crops and other
vegetation, of historical records of floods and droughts, and
indeed of everything else that has ever been recorded or
remembered, and then to apply to this everything that is known
about meteorology, plant physiology, soil physics, hydrogeology,
sediment transport and everything else that is relevant within this
context. Of course, no matter how much data we have and no matter
how much we know, it will never be enough to treat some problems
and some situations, but still we can aim in this way to do the
best that we possibly can.
This is a comprehensive work of reference for engineers dealing
with the hydraulic problems that occur along coastlines and
estuaries and in harbours. This branch of engineering has
experienced rapid and profound changes since the 1960s due to the
introduction of powerful computer modelling techniques. The book
presents concise reviews of key topics on these techniques as well
as the traditional civil engineering aspects of design and
construction of coastal and maritime works. The powerful tools
which are now available for computational and numerical modelling
of hydraulic systems have to a considerable extent replaced
physical models as the most appropriate means of investigating and
selecting economic design options. This development has taken place
alongside a greater understanding of the transport processes of
granular and cohesive sediments, and an increasing concern with the
environmental impact of engineering works. At the design stage, the
engineer now commonly has to demonstrate the impact of the proposed
works on the natural/watery environment. The chapters are presented
under seven main headings: the physical environment; the scientific
background; numerical tools and t
A major new reference book bringing together wide-ranging expert
guidance on coastal engineering, including harbours and estuaries.
It covers both traditional engineering topics and the fast
developing areas of mathematical modelling and computer simulation.
This revised text provides an updated account of principles and
survey modelling in hydraulic, coastal and offshore engineering.
Topics covered include discrete forms of conservation laws,
numerical methods, the foundations of computational hydraulics, and
applications of computational hydraulics.
It is the task of the engineer, as of any other professional
person, to do everything that is reasonably possible to analyse the
difficulties with which his or her client is confronted, and on
this basis to design solutions and implement these in practice. The
distributed hydrological model is, correspondingly, the means for
doing everything that is reasonably possible - of mobilising as
much data and testing it with as much knowledge as is economically
feasible - for the purpose of analysing problems and of designing
and implementing remedial measures in the case of difficulties
arising within the hydrological cycle. Thus the aim of distributed
hydrologic modelling is to make the fullest use of cartographic
data, of geological data, of satellite data, of stream discharge
measurements, of borehole data, of observations of crops and other
vegetation, of historical records of floods and droughts, and
indeed of everything else that has ever been recorded or
remembered, and then to apply to this everything that is known
about meteorology, plant physiology, soil physics, hydrogeology,
sediment transport and everything else that is relevant within this
context. Of course, no matter how much data we have and no matter
how much we know, it will never be enough to treat some problems
and some situations, but still we can aim in this way to do the
best that we possibly can.
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