2011
DOI: 10.9765/kscoe.2011.23.3.226
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Downtime Analysis for Pohang New Harbor through Long-term Investigation of Waves and Winds

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Cited by 11 publications
(6 citation statements)
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“…In the figure, small wavy undulations are observed in all the curves over the frequency ranges corresponding to infragravity waves. According to previous studies on wave observation at other locations on the Korean east coast [22][23][24], such undulations either have different patterns depending on the locations or are not even observed at some locations. For this reason, these undulations are presumed to be caused by regional effects such as reflections from the coast, which explains why the undulations are very similar for all curves.…”
Section: Separation Period Of Infragravity Wavesmentioning
confidence: 99%
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“…In the figure, small wavy undulations are observed in all the curves over the frequency ranges corresponding to infragravity waves. According to previous studies on wave observation at other locations on the Korean east coast [22][23][24], such undulations either have different patterns depending on the locations or are not even observed at some locations. For this reason, these undulations are presumed to be caused by regional effects such as reflections from the coast, which explains why the undulations are very similar for all curves.…”
Section: Separation Period Of Infragravity Wavesmentioning
confidence: 99%
“…Considering this, it is quite natural that the magnitude of infragravity waves can be different depending on the choice of the separation period [8,[22][23][24]. In fact, the heights and periods of infragravity waves observed at Sokcho beach on the Korean east coast were apparently different depending on the use of different separation periods of 20, 25 and 30 s. In contrast, the upper limit, or higher cutoff period of infragravity waves, had little decisive influence on the magnitude of infragravity waves [25].…”
Section: Introductionmentioning
confidence: 99%
“…In this study, the CGWAVE model is applied to Pohang New Harbor in order to simulate harbor resonance and to verify the model against field measurement wave data (Jeong et al, 2011). The simulation domain is 13.5 km in the offshore direction and 9.5 km in the longshore direction.…”
Section: Numerical Simulation Conditionsmentioning
confidence: 99%
“…. 따라서 이런 단주기파의 항내 침입을 효 과적으로 차단할 경우 항내정온도 문제가 개선될 수 있을 것으 로 제안되었다 (Jeong et al, 2011;Pohang Regional Maritime Affairs andPort Office, 2010, 2012 (Fig. 3(b)).…”
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