Tidal propagation in an oceanic island with sloping beaches
| dc.citation.epage | 1351 | en_US |
| dc.citation.issue | 7 | en_US |
| dc.citation.spage | 1341 | en_US |
| dc.citation.volume | 14 | en_US |
| dc.citation.woscount | 3 | |
| dc.contributor.author | Chang, Y. -C. | en_US |
| dc.contributor.author | Jeng, D-S | en_US |
| dc.contributor.author | Yeh, H. -D. | en_US |
| dc.contributor.department | 環境工程研究所 | zh_TW |
| dc.contributor.department | Institute of Environmental Engineering | en_US |
| dc.date.accessioned | 2014-12-08T15:07:53Z | |
| dc.date.available | 2014-12-08T15:07:53Z | |
| dc.date.issued | 2010 | en_US |
| dc.description.abstract | In this study, a new analytical solution for describing the tide-induced groundwater fluctuations in oceanic islands with finite length and different slopes of the beaches is developed. Unlike previous solutions, the present solution is not only applicable for a semi-infinite coastal aquifer, but also for an oceanic island with finite length and different sloping beaches. The solution can be used to investigate the effect of higher-order components and beach slopes on the water table fluctuations. The results demonstrate the effect of higher-order components increases with the shallow water parameter or amplitude parameter and the water table level increases as beach slopes decrease. | en_US |
| dc.identifier.doi | 10.5194/hess-14-1341-2010 | en_US |
| dc.identifier.issn | 1027-5606 | en_US |
| dc.identifier.journal | HYDROLOGY AND EARTH SYSTEM SCIENCES | en_US |
| dc.identifier.uri | http://dx.doi.org/10.5194/hess-14-1341-2010 | en_US |
| dc.identifier.uri | https://ir.lib.nycu.edu.tw/handle/11536/6200 | |
| dc.identifier.wosnumber | WOS:000280515100016 | |
| dc.language.iso | en_US | en_US |
| dc.title | Tidal propagation in an oceanic island with sloping beaches | en_US |
| dc.type | Article | en_US |