DC Field | Value | Language |
---|---|---|
dc.contributor.author | Won, Sang In | ko |
dc.contributor.author | Kim, Sung Yong | ko |
dc.date.accessioned | 2018-09-18T03:54:08Z | - |
dc.date.available | 2018-09-18T03:54:08Z | - |
dc.date.created | 2018-08-27 | - |
dc.date.created | 2018-08-27 | - |
dc.date.issued | 2018-06-05 | - |
dc.identifier.citation | AOGS (Asia Oceania Geosciences Society) 2018 | - |
dc.identifier.uri | http://hdl.handle.net/10203/245252 | - |
dc.description.abstract | This paper examines surface tidal and residual circulations in an enclosed bay, Yeosu Bay off the southern coast of Korea using observations of hourly high-frequency radar(HFR)-derived surface current maps on a spatial resolution of 1 km and hourly records of the local sea surface height and wind for a period of two years (2015 to 2016) and analytic solutions obtained from an idealized tidal model. The phase structure of the semi-diurnal ($M_{2}$) surface currents is more homogeneous and uniform than that of the diurnal ($K_{1}$) surface currents, and the variance ratios of residual surface currents in the semi-diurnal frequency band [$1.91 \leq \sigma \leq 1.95$ cycles per day (cpd)] are approximately 50$\%$ less than those of residuals in the diurnal frequency band ($0.98 \leq \sigma \leq 1.02$ cpd) including $P_{1}$, $S_{1}$, and $K_{1}$ tidal constituents. These two characteristics may indicate that the regional surface circulation is more barotropic at the semi-diurnal frequency and more baroclinic at the diurnal frequency. | - |
dc.language | English | - |
dc.publisher | Asia Oceania Geosciences Society | - |
dc.title | Surface tidal and residual circulations in an enclosed bay | - |
dc.type | Conference | - |
dc.type.rims | CONF | - |
dc.citation.publicationname | AOGS (Asia Oceania Geosciences Society) 2018 | - |
dc.identifier.conferencecountry | US | - |
dc.identifier.conferencelocation | Hawaii Convention Centre | - |
dc.contributor.localauthor | Kim, Sung Yong | - |
dc.contributor.nonIdAuthor | Won, Sang In | - |
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