새만금해역에서 몬순과 방조제에 의한 모래의 급속한 이동 연구
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | 이희준 | - |
| dc.contributor.author | 이석 | - |
| dc.date.accessioned | 2020-07-17T00:51:59Z | - |
| dc.date.available | 2020-07-17T00:51:59Z | - |
| dc.date.created | 2020-02-11 | - |
| dc.date.issued | 2008-06-17 | - |
| dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/29891 | - |
| dc.description.abstract | The eastern Yellow Sea is predominantly governed by the monsoonal climate that isresponsible for harsh winter with high waves and wind-generated currentssuperimposed on tidal currents and mild summer with tidal currents only. Geologicalinvestigations conducted over a vast area offshore a giant dyke, Saemangeum,indicate that sands prominently moved southward by about 3 km during a shortperiod of 3 years since the dyke construction. This resulted from combined effects of the dyke construction and monsoonal seasonality. The emplacement of the dyke with its alignment of NE-SW has forced the major axis of tidal currents offshore to rotate about 40o | - |
| dc.description.uri | 1 | - |
| dc.language | English | - |
| dc.publisher | Asia Oceania Geosciences Society | - |
| dc.relation.isPartOf | AOGS 5th Annual Meeting | - |
| dc.title | 새만금해역에서 몬순과 방조제에 의한 모래의 급속한 이동 연구 | - |
| dc.title.alternative | Interplay of an Artificial Dyke And Monsoonal Seasonality in Reinforcing Underwater Sand Movements in The Mid-West Coast of Korea | - |
| dc.type | Conference | - |
| dc.citation.conferencePlace | KO | - |
| dc.citation.endPage | 1 | - |
| dc.citation.startPage | 1 | - |
| dc.citation.title | AOGS 5th Annual Meeting | - |
| dc.contributor.alternativeName | 이희준 | - |
| dc.contributor.alternativeName | 이석 | - |
| dc.identifier.bibliographicCitation | AOGS 5th Annual Meeting, pp.1 | - |
| dc.description.journalClass | 1 | - |
- Appears in Collections:
- Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
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