The paper deals with the conformal mapping of finite, plane, simply connected
domains, representing oceans, lakes, estuaries, bays, lagoons, and other natural
water bodies of this kind. As a rule, they are bounded by geometrically complex
shorelines. The partial differential problems investigated in Oceanology and posed
in such domains have turned out to be difficult to solve for at least three reasons. They follow on from the mathematical properties of the differential equations
governing such problems, from the just-mentioned geometrical complexity of
the domains of solution, and from the sensitivity of the solutions to boundary
conditions.
In view of the last reason the contours admitted as boundaries of the domains
of the solution ought to be as close to the real shorelines as possible. The
obviously inaccurate approximation of the shorelines by ‘staircases’, which appears
rather often (cf. Catewicz & Jankowski 1983, Lin & Chandler-Wilde 1996) as
a consequence of applying finite difference methods to the solution of the partial
differential problems, raises serious doubts from the point of view of Numerical
Fluid Mechanics.
It is recalled in the paper that such inaccuracies are not unavoidable: that
complicated plane domains can be transformed accurately by means of properly
applied conformal mapping onto regular, canonical domains – in particular, onto
discs or squares. Such a transformation is demonstrated on the rather difficult
example of the Vistula Lagoon. The transformation begins with the decomposition
of the domain into five plane subdomains, each one of which is eventually
transformed onto a disc. Every such result is arrived at quite independently of
the remaining subdomains, by means of a set of properly selected consecutive
mappings. Hence, the final canonical domain consists in this case of a system of
five discs which, however, within the framework of this differential problem, have to
be treated as interconnected. The interconnections involve images of four segments
of straight lines, separating the original subdomains.
The transformations and the resulting canonical domain presented in the paper
are intended to be applied to the solution of certain hydrodynamical problems
concerning the Vistula Lagoon, which will be published elsewhere.
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