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of 64
pro vyhledávání: '"B. Vreugdenhil"'
Autor:
W. van Aalst, P. Piscaer, B. Vreugdenhil, F. Bouman, M. van Antwerpen, G. van Antwerpen, J. Baan
Publikováno v:
Roads and Airports Pavement Surface Characteristics ISBN: 9781003429258
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c0d08617314d11fe30141164e1f1185
https://doi.org/10.1201/9781003429258-38
https://doi.org/10.1201/9781003429258-38
Akademický článek
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Autor:
Cornelis B. Vreugdenhil
What is Computational Hydraulics? Computational hydraulics is one of the many fields of science in which the application of computers gives rise to a new way of working, which is intermediate between purely theoretical and experimental. It is concern
Publikováno v:
Journal of Physical Oceanography. 25:2141-2154
Diagnostic equations relating the zonally averaged overturning circulation to north–south density variations are derived and used to determine a new closure scheme for use in zonally averaged ocean models. The presentation clarifies the dynamical l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1299e666ba34d3f0cae8fcacebe1bee0
https://doi.org/10.1175/1520-0485(1995)025<2141:vdazao>2.0.co
https://doi.org/10.1175/1520-0485(1995)025<2141:vdazao>2.0.co
Autor:
C. B. Vreugdenhil
Publikováno v:
Communications in Applied Numerical Methods. 7:633-637
A relation is given between grid properties such as grid angle and aspect ratio and the metric coefficients of the transformation from the physical to the computational domain. A transformation is proposed in which these grid properties occur explici
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17c97cc4ff115a0df29b100da68946b9
https://doi.org/10.1002/cnm.1630070810
https://doi.org/10.1002/cnm.1630070810
Akademický článek
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Autor:
C. B. Vreugdenhil
Publikováno v:
Water Science and Technology Library ISBN: 9789048144723
For the standard methods of time discretization, discussed in sections 8.2 and 8.3, the numerical accuracy for linear wave propagation can be studied using the finite-difference analogue of (7.1): $$\textup{v}^{n}=\rho ^{n}\;exp(ik_{1}x+ik_{2}y)\text
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::64e1abde15b5bf976c72d0572c98d743
https://doi.org/10.1007/978-94-015-8354-1_9
https://doi.org/10.1007/978-94-015-8354-1_9
Autor:
C. B. Vreugdenhil
Publikováno v:
Water Science and Technology Library ISBN: 9789048144723
Shallow-water flow might seem to be a too special subject to devote a complete book to, but it is actually quite common. Many types of flow, not necessarily involving water as a fluid, can be characterized as shallow-water flows. The general characte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5f59166d7d21acc6d136c9f04a8e1f1
https://doi.org/10.1007/978-94-015-8354-1_1
https://doi.org/10.1007/978-94-015-8354-1_1
Autor:
C. B. Vreugdenhil
Publikováno v:
Water Science and Technology Library ISBN: 9789048144723
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2cce86134970fc7d6e64e30075b2f6e
https://doi.org/10.1007/978-94-015-8354-1_7
https://doi.org/10.1007/978-94-015-8354-1_7
Autor:
C. B. Vreugdenhil
Publikováno v:
Water Science and Technology Library ISBN: 9789048144723
Most of this book is about 2-d shallow-water flows, obtained either by integrating over depth or by splitting into vertical modes. This approach works remarkably well in many cases, even when you would expect significant 3-d effects, such as in wind-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd2e5a0d733e99e21374c7ed9abab3d3
https://doi.org/10.1007/978-94-015-8354-1_11
https://doi.org/10.1007/978-94-015-8354-1_11