• 한국해양공학회지
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• 제20권3호
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• pp.45-53
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• 2006

Each year, the south coast of Korea is badly damaged from storm surge. The damages are greatly dependent upon the local peculiarities of the region where the storm surge occurs. So, in order to prevent/reduce recurrence of the disaster, it is very important to investigate the fluctuation characteristics of the storm surge height, related to the local peculiarities at each coastal area where occurrence of the disaster is expected. In this paper, using the numerical model, the storm surge was simulated to examine its fluctuation characteristics at the Gyeongnam coast (southeast coast of Korea). Typhoons of Sarah (5914), Thelma (8705) and Maemi (0314), which caused terrible damage to the coastal area in the southeast coast of Korea in the past, were used forstorm surge simulations. Moreover, the storm surge due to virtual typhoons, which were combined the characteristics of each proposed typhoons (Maemi, Sarah, Thelma)with the travel route of other typhoon, was predicted. As expected, the results revealed that the storm surge heights are enhanced at the coastal regions with the concavity like a long-shaped bay. Also, the storm surge heights, due to each typhoon, were compared and discussed at major points along the Gyeongnam coast, related to the local peculiarities, as well as the characteristics and the travel route of typhoon.

• Earthquakes and Structures
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• 제15권6호
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• pp.605-616
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• 2018

In this paper, an extended Cloud analysis method is developed for seismic fragility assessment of existing highway bridges in the southeast Queensland region. This method extends the original Cloud analysis dataset by performing scaled Cloud analyses. The original and scaled Cloud datasets are then paired to generate seismic fragility curves. The seismic hazard in this region is critically reviewed, and the ground motion records are selected for the time-history analysis based on various record selection criteria. A parametric highway bridge model is developed in the OpenSees analysis software, and a sampling technique is employed to quantify the uncertainties of highway bridges ubiquitous in this region. Technical recommendations are also given for the seismic performance evaluation of highway bridges in such low-to-moderate seismic zones. Finally, a probabilistic fragility study is conducted by performing a total of 8000 time-history analyses and representative bridge fragility curves are generated. It is illustrated that the seismic fragility curves generated by the proposed extended Cloud analysis method are in close agreement with those which are obtained by the rigorous incremental dynamic analysis method. Also, it reveals that more than 50% of highway bridges existing in southeast Queensland will be damaged subject to a peak ground acceleration of 0.14 g.

• 한국해양학회지
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• 제9권1_2호
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• pp.10-18
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• 1974

The cold water mass around the southeast coast of the Korean Peninsula is analyzed by using CSK data from 1966 through 1970. It is shown that this water mass flows down from the region offshore of Jukbyun to the area of Youngil Bay along the 100meter contour line of bottom topography. In ordinary summer conditions when the current velocity in the Korea Strait is usually above about 50cm/sec and the wind direction is southwest, the cold water ascends to the surface and makes the surface temperature gradient large, unless disturbed by a tropical cyclon. The bottom water of the Korea Strait is formed by the stratification after the Tsushima intermediate water and the Japan Sea intermediate water have been mixed. In winter the Tsushima intermediate water with high salinity sinks rapidly around the inlet of the Japan Sea and prevents the Japan Sea intemediate water from entering the Korea Strait.

• 한국해양공학회지
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• 제27권4호
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• pp.33-44
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• 2013

IIn this study, a wave-surge-tide coupling numerical model was developed to consider nonlinear interaction. Then, this model was applied and calculations were made for a storm surge on the southeast coast. The southeast coast was damaged by typhoon "Maemi" in 2003. In this study, we used a nearshore wind wave model called SWAN (Simulating WAves Nearshore). In addition, the Meyer model was used for the typhoon model, along with an ocean circulation model called POM (Princeton Ocean Model). The wave-surge-tide coupling numerical model could calculate exact parameters when each model was changed to consider the nonlinear interaction.

• Journal of East-Asian Urban History
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• 제3권1호
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• pp.139-160
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• 2021

The verandah was a common feature of Chinese multi-storeyed houses in Southeast Asia and China. This paper argues that while an earlier version of a narrow walkway might have had its origin in Singapore, the building of an extension on the upper floors encroaching the airspace over the road skirting the building was an arrangement allowed by the colonial Hong Kong government in compensation to landlords for space devoted to ventilation. As the introduction of reinforced concrete allowed buildings to become taller, the more attractive it was to developers to incorporate the verandah design.

• 대한지리학회지
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• 제38권4호
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• pp.490-504
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• 2003

한반도 남동해안의 감포와 중부 동해안 정동진에서 발견된 해안단구 고고위I면과 고고위II면을 울산-경주 경계지역 지경리 일대에서 재차 확인하였다. 특히 이곳에는 현재까지 우리나라에서 보고된 해발고도가 가장 높은 해안단구인 구정선고도 140m보다 한 단 더 높은 해발고도 155m인 고고위 지경(HH JK)면이 분포한다. 따라서 지경리지역 고고위면의 구정선고도는 해발고도 155m, 140m, l15m로 측정되었고, 형성시기는 각각 MIS 17(72∼69만년 BP), MIS 15(63∼56만년 BP)와 MIS 13(51∼48만년 BP)으로 편년되었다. 또한 고고위면의 규모가 매우 큰 것은 기반암과 고고위면 형성시 해안 지형의 특성에 기인하는 것으로 생각된다. 동해안 중부와 남부에서 고고위면을 비롯한 고위면, 중위면, 저위면의 구정선고도체계가 같으므로, Pleistocene 중기 이후 동해안에는 남북간 지반융기량의 차이가 존재하지 않는다. 해안단구 고고위 지경면, 고고위 I면, 고고위 II면, 고위 I면, 고위 II면의 구정선고도와 형성시기와의 관계로부터 얻은 동해안지역 지반 융기속도는 0.23mm/y로 거의 균일하다.

• Fisheries and Aquatic Sciences
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• 제16권4호
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• pp.325-329
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• 2013

New occurrences in Korean waters were recorded for two penaeid species: Atypopenaeus stenodactylus (Stimpson, 1860) and Metapenaeopsis toloensis Hall, 1962, which were previously known from the Indo-West Pacific up to southern Japan. The specimens were collected from the southeastern coast of Korea by a shrimp beam trawl. The former is the only known member of the genus Atypopenaeus and the latter is the sixth species of the genus Metapenaeopsis reported in Korea. Morphological descriptions and illustrations with color photographs of the specimens are given. At present, the Korean Penaeidae consist of 20 species in 11 genera. A key to the Korean genera of family Penaeidae is also presented.

• Animal Systematics, Evolution and Diversity
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• 제29권2호
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• pp.115-128
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• 2013

Five scyllarine lobster species, belonging to the family Scyllaridae, are described from Korean waters: Chelarctus cultrifer (Ortmann, 1897), Crenarctus bicuspidatus (De Man, 1905), Galearctus kitanoviriosus (Harada, 1962), G. timidus (Holthuis, 1960), and Petrarctus brevicornis (Holthuis, 1946). Of these, three species, C. bicuspidatus, G. timidus, and P. brevicornis are new to Korean marine carcinological fauna. This report extends the known range of G. timidus to the southern coast of Korea from Taiwan in the East China Sea. Excluding C. bicuspidatus and G. kitanoviriosus, the other three species are relatively rare in Korean waters. They are described herein with color photographs, and a key to the Korean genera and species of Scyllarinae is also presented.

• Fisheries and Aquatic Sciences
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• 제16권3호
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• pp.199-205
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• 2013

Three species of pelagic sergestid shrimps, Deosergestes seminudus (Hansen, 1919), Sergia lucens (Hansen, 1922) and S. talismani (Barnard, 1947), were identified based on collections by the National Fisheries Research and Development Institute from the Korean coast of the Yellow Sea between 2003 and 2011. They are herein reported for the first time from the Yellow Sea. Morphological descriptions and illustrations with color photographs of all species are also given. With the addition of these species, the family Sergestidae in the Korean waters now comprises five species belonging to three genera. Finally, a key to the Korean genus and species of the family Sergestidae is presented.

• 해양환경안전학회지
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• 제22권7호
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• pp.836-845
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• 2016

본 연구에서는 하계 한국 남동해 간절곶 주변해역의 냉수대 구조와 변동을 CTD 관측과 수층별 수온 장기 연속 모니터링 자료를 이용하여 분석하였다. 냉수대의 표층수온은 냉수기 이전과 $-12^{\circ}C$의 차이를 보였으며 해저지형 효과로 간절곶에서 냉수대 세력이 가장 컸다. 남북해역 간 등온선의 시계열분포에 간절곶을 경계로 공간변화가 발생해 간절곶 주변 해저지형이 언덕(hill)역할을 하고 있음이 추정되었다. 냉수대는 해안에 평행한 풍속이 양(+)의 값일 때 출현하는 연안용승반응을 나타냈고, 수온의 감소와 상승은 풍향이 바뀐 후 하루 이내에 반응하였다. 간절곶 주변은 얕은 수심 주위에서 발생하는 와류효과가 결합하여 바람에 의한 용승효과가 강화되었다. 수온변화는 2~6일 주기의 바람변동에 민감하였으며, 수온감소는 12~36시간의 위상차를 나타냈다. 냉수대가 출현한 7월은 2~3일 주기, 8월은 3~8일 주기에서 바람-수온변화의 상관성이 컸다.