- Tytuł:
- Conformal mapping of the Gulf of Gdańsk onto a canonical domain
- Autorzy:
-
Czesnik, P.P.
Prosnak, W.J. - Powiązania:
- https://bibliotekanauki.pl/articles/48629.pdf
- Data publikacji:
- 2002
- Wydawca:
- Polska Akademia Nauk. Instytut Oceanologii PAN
- Tematy:
-
Schwarz-Christoffel function
solution
conformal mapping
shoreline
Gdansk Gulf
inversion - Opis:
-
The paper deals with the conformal mapping of a plane, finite, simply connected
domain, representing the southern segment of the Gulf of Gdańsk, enclosed from
the North by a parallel, tangential to Cape Rozewie. The segment contains the
Hel Peninsula.
The method of double decomposition, presented in Prosnak & Cześnik (2001),
is applied to the transformation of such an original domain onto a canonical one,
which consists of two separate unit discs.
The first decomposition concerns the domain which is split into two adjacent
subdomains by means of a segment of a straight line.
The second decomposition involves two holomorphic functions, each one
mapping a subdomain onto a separate disc. The decomposition consists in replacing
the function by a sequence of simple ones, so that the mapping is performed
step-wise. Each sequence starts with the Schwarz-Christoffel function, the last step
consisting in an inversion that transforms an infinite circular domain onto a disc.
The data for the problem is contained in the Annex, and is represented by two
sets of rectangular coordinates defining consecutive discrete points of the contours
bounding the subdomains.
The solution to the problem consists of:
– two sets of functions, consecutively transforming each of the subdomains;
– the numerical values of the parameters of these functions;
– a set of figures illustrating the consecutive transformations. The accuracy of the first, and of the penultimate transformation are given, because only in the case of these two functions do the unknown coefficients have to be determined by means of a suitable iterative process. The coefficients of all the remaining functions are evaluated from exact formulae. It should be recalled that the depth of the Gulf of Gdańsk varies considerably – from a few to 110 metres – the gradients of the bottom being rather large. Therefore, the domain of the solution for any mathematical problem describing the hydrodynamical phenomena occurring in the Gulf is usually taken to be three-dimensional. Nevertheless, the paper deals with the transformation of the free surface of the Gulf, assumed as plane. It should be emphasized that this assumption does not mean that the whole domain of the solution has to be regarded as plane. - Źródło:
-
Oceanologia; 2002, 44, 2
0078-3234 - Pojawia się w:
- Oceanologia
- Dostawca treści:
- Biblioteka Nauki
Artykuł