dc.contributor.author |
Christodoulou George, C |
en |
dc.contributor.author |
Kouloumbis Athanassios, E |
en |
dc.contributor.author |
Aza Alice, O |
en |
dc.date.accessioned |
2014-03-01T02:47:47Z |
|
dc.date.available |
2014-03-01T02:47:47Z |
|
dc.date.issued |
1987 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/33345 |
|
dc.relation.uri |
http://www.scopus.com/inward/record.url?eid=2-s2.0-0023266848&partnerID=40&md5=d166a24492156a7a05c3563b9b4e01c7 |
en |
dc.subject.other |
MATHEMATICAL TECHNIQUES - Finite Element Method |
en |
dc.subject.other |
TIDES |
en |
dc.subject.other |
COARSE GRID |
en |
dc.subject.other |
COMPOUND TIDE |
en |
dc.subject.other |
FINE GRID |
en |
dc.subject.other |
HYDRODYNAMIC CIRCULATION |
en |
dc.subject.other |
HYDRODYNAMICS |
en |
dc.title |
2-D CIRCULATION IN THE SARONIC GULF. |
en |
heal.type |
conferenceItem |
en |
heal.publicationDate |
1987 |
en |
heal.abstract |
The paper refers to mathematical modeling of the 2-D hydrodynamic circulation in the Saronic Gulf, in Greece. The finite element method is followed to evaluate the flow behaviour. Two grids are employed, a coarse one for initial model adaptation and a finer one for a more detailed study of circulation patterns. Actual tide data are obtained at the boundary of the domain and a typical compound tide is introduced; however residual tidal currents are found to be negligible. Further work proceeds towards quantitative verification of the model in connection with the proper description of forcing mechanisms and their superposition. |
en |
heal.publisher |
ASCE, New York, NY, USA |
en |
heal.journalName |
Proceedings of the Coastal Engineering Conference |
en |
dc.identifier.volume |
3 |
en |
dc.identifier.spage |
2477 |
en |
dc.identifier.epage |
2490 |
en |