• Journal of Navigation and Port Research
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• v.30 no.3 s.109
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• pp.253-258
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• 2006

In this paper, we analyse the marine leisure base condition of the archipelago at the southwest sea area which has the natural advantage for marine leisure. We also discuss how to adapt the yacht business on the above area. At first, we analyse the current situation of the domestic marine leisure and draw up a plan to solve its problem. Finally we apply an environment friendly marina establishment to the archipelago at the southwest sea area and evaluate its validity.

• 공원문화
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• s.9
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• pp.41-41
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• 1978

한국국립공원협회는 우리나라에서 특수한 경관과 자연 여건을 지닌 다도해의 자연성과 개발 타당성 조사를 실시하였는데 그 개요를 소개한다.

• 어항어장
• /
• s.21
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• pp.39-42
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• 1992

• Proceedings of the Korean Institute of Navigation and Port Research Conference
• /
• 2004.11a
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• pp.197-202
• /
• 2004

In this paper, we tackled the marine leisure business of the archipelago at the southwest sea area which has the natural advantage for marine leisure. We also discuss how to adapt the yacht business on the above area. At first, we will introduce the predominant case on the marine leisure business of the overseas. Next we will analyze the current situation of the domestic marine leisure and draw up a plan to solve its problem. Finally we apply an environment friendly marina establishment to the archipelago at the southwest sea area and evaluate its validity.

• 공원문화
• /
• s.19
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• pp.47-48
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• 1981

• 공원문화
• /
• s.76
• /
• pp.50-68
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• 1999

• 공원문화
• /
• s.11
• /
• pp.7-22
• /
• 1979

• 공원문화
• /
• s.22
• /
• pp.43-51
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• 1982

• 공원문화
• /
• s.23
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• pp.45-49
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• 1983

• Journal of the Korean Society of Marine Environment & Safety
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• v.24 no.2
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• pp.179-187
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• 2018

In order to understand the flow of currents around Aphae Island and the surrounding Archipelago, the numerical model experiments on tidal currents and tide-induced residual currents were carried out. Dominant semidiurnal tidal currents have a reversing form and flow along the narrow channels of the archipelago. During periods of flood, currents flow from the west of Hwawon Peninsula to the archipelago to the northwest together with the currents flowing from the channels at Palgeum Island to Amtae Island and Amtae Island to Jeung Island. Ebb currents flow from the northwest archipelago to the channel of Amtae Island and Jeung Island as well as Amtae Island to Palgeum Island, further flowing south between Palgeum Island and Hwawon Peninsula. Flood currents are separated from east and west at the southern coast of Aphae Island, but flow south from both the west and east of Aphae Island to the channel found between Palgeum Island and Hwawon Peninsula at ebb. Flow speed is high between Amtae Island and Aphae Island where the flows meet and join. Lee wakes or topographical eddies are formed around the islands due to the high speed of the currents flowing along the narrow channel in the archipelago, manifesting as a tide-induced residual current. A weak cyclonic wake and anti-cyclonic eddy both exist at the west and northwestern coast of Aphae Island individually. The speed of the tide-induced residual current become slow on account of the wide littoral zone at exists around Aphae Island.