dc.contributor.author |
Melas, D |
en |
dc.contributor.author |
Ziomas, I |
en |
dc.contributor.author |
Zerefos, C |
en |
dc.date.accessioned |
2014-03-01T01:43:05Z |
|
dc.date.available |
2014-03-01T01:43:05Z |
|
dc.date.issued |
1995 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/24029 |
|
dc.subject |
Boundary Layer |
en |
dc.subject |
Complex Terrain |
en |
dc.subject |
Coordinate System |
en |
dc.subject |
Diurnal Variation |
en |
dc.subject |
Numerical Model |
en |
dc.subject |
Sea Breeze |
en |
dc.subject |
Three Dimensional |
en |
dc.subject |
Growth Rate |
en |
dc.subject |
Higher Order |
en |
dc.title |
Boundary layer dynamics in an urban coastal environment under sea breeze conditions |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1016/1352-2310(95)00140-T |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1016/1352-2310(95)00140-T |
en |
heal.publicationDate |
1995 |
en |
heal.abstract |
A three-dimensional, higher-order turbulence closure model is applied to simulate the boundary layer dynamics in Attica peninsula, where the city of Athens is located. All model equations are transformed to a terrain influenced coordinate system, which enables studies of flow over complex terrain. Major characteristics of the sea breeze circulation including vertical extension and intensity as well as the growth |
en |
heal.journalName |
Atmospheric Environment |
en |
dc.identifier.doi |
10.1016/1352-2310(95)00140-T |
en |