• 제목, 요약, 키워드: Tide age

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제주 연안의 소대망에서 조석에 의한 어획량 변동 (Catch fluctuation of the Pound Set Net According to Tide Age in the Coastal Waters of Jeju)

  • 김병엽;서두옥;이창헌
    • 한국수산과학회지
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    • v.42 no.1
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    • pp.83-88
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    • 2009
  • The purpose of this paper is to obtain the fundamental data on the catch fluctuation in the pound set net according to the tide age from the catch recorded from the year 1997 to 2004 in the coastal waters of Guideok, Jeju. Total catch by the pound set net had a little connection with the tide age. During increasing tide, total catch were reduced slightly from the neap tide to the high tide while there seemed to be a little sign of rise in the total catch until decreasing tide. But in the relation between the catches and the tide age, the level of the correlation coefficient chosen at $p{\le}0.05$ was not significant. Therefore, the catch of the pound set net seemed not to be influenced by the tide age. In addition, CPUE at the high tide was higher than that at the neap tide. When the catch per operating frequency was graded in the order under 50 kg, 50-100 kg and 100-200 kg, the frequency rate by the pound set net was 38%, 19% and 19%, respectively.

제주연안 각망의 조석에 의한 어획량 변동 (Catch fluctuation of the rectangular set net according to the tide age in the coastal waters of Jeju)

  • 이창헌;최찬문
    • 수산해양기술연구
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    • v.44 no.2
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    • pp.112-119
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    • 2008
  • The fundamental data on the catch fluctuation in the rectangular set net according to the tide age were developed based on the catches recorded from the year 1986 to 2004 in the coastal waters of Hamdeok, Jeju. Total catch by the rectangular set net had a deep connection with the tide age. In particular, during increasing tide, total catch were reduced gradually from the neap tide to the high tide. As it turned out, the slope of total catch declined by degree and showed a correlation coefficient of determination of 0.76. On the contrary, in the case of decreasing tide, there was little sign of rise in total catch. In particular, large catch seemed to occur at the next tide to the neap tide. In the relation between the catch and the tide age, the level of the correlation coefficient chosen at $p{\leq}0.05$ decreased in the order rabbitfish(-0.84) and horse mackerel(-0.71), while the significance of other dominant species were not selected.

여수연안 낙지주낙 어장의 해황과 어획 변동에 관한 연구 (2) (Influence of Sea Condition on Catch Fluctuation of Long Line for Common Octopus, Octopus Variddilis, in the Coastal Waters of Yosu (2))

  • 정정민;김동수
    • 수산해양기술연구
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    • v.37 no.3
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    • pp.159-162
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    • 2001
  • 낙지 주낙 어장의 환경요인이 어획량에 미치는 영향을 조사하기 위하여 1997년 1월부터 7월까지 여수연안에서 수온, 염분, 밀도, 풍향, 풍속등과 어획량을 각각 조사하고 이들을 서로 비교 분석한 결과를 요약하면 다음과 같다. 1) 풍향별 어획량은 남동풍일 때 가장 많았고 북서풍일 때 가장 적었으며, 풍속별 어획량은 2일 때 가장 많았고 그보다 커질 경우는 감소하였다. 2) 물때별 단위 노력당 어획량은 15물에서 가장 많고 4물에서 가장 적으며. 조류가 차차 약해지는 11∼14물 사이의 어획량이 조류가 차차 강해지는 1∼4물 사이의 어획량보다 많았다. 3) 썰물과 밀물 때의 어획량은 간조에서 만조로 바뀐 후 1시간 동안의 구간, 즉 간조에서 물이 들기 시작한지 1시간 동안에 어획량이 가장 많았고. 썰물 시각대 보다는 밀물 시각대에 어획량이 비교적 많은 경향이었다

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여수연안 낙지주낙 어장의 해황과 어획 변동에 관한 연구(2) (Influence of Sea Condition on Catch Fluctuation of Long Line for Common Octopus, Octopus Variddilis, in the Coastal Waters of Yosu (2))

  • 정정민;김동수
    • 수산해양기술연구
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    • v.37 no.4
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    • pp.326-330
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    • 2001
  • 낙지주낙 어장의 환경요인이 어획량에 미치는 영향을 조사하기 위하여 1997년 1월부터 7월까지 여수연안에서 풍향, 풍속, 물때별 및 조업 시각대별로 어획량을 각각 사하고 이들을 서로 비교 분석한 결과를 요약하면 다음과 같다. 1) 풍향별 어획량은 남동풍일 때 가장 많았고 북서풍일 때 가장 적었으며, 풍속별 어획량은 2일 때 가장 많았고 그보다 커질 경우는 감소하였다. 2) 물때별 단위 노력당 어획량은 15물에서 가장 많고 4물에서 가장 적으며, 조류가 차차 약해지는 11∼14물 사이의 어획량이 조류가 차차 강해지는 1∼4물 사이의 어획량보다 많았다. 3) 썰물과 밀물 때의 어획량은 간조에서 만조로 바뀐 후 1시간 동안의 구간, 즉 간조에서 물이 들기 시작한지 1시간 동안에 어획량이 가장 많았고, 썰물 시각대 보다는 밀물 시각대에 어획량이 비교적 많은 경향이었다.

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인천항의 조석, 조류 및 조량에 대하여 (On the Tides, Tidal Currents and Tidal Prisms at Inchon Harbor)

  • 이석우
    • 한국해양학회지
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    • v.7 no.2
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    • pp.86-97
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    • 1972
  • The tides, tidal currents and tidal prisms at Inchon Harbor are studied with recent data. The tides at Inchon Harbor is of semi-diurnal type having a spring range of 798cm and a phase age of 2 days. The monthly mean sea level at Inchon has a maximum at August and a minimum at January with a annual range of about 40cm. the tidal currents at Inchon Outer Harbor are of semi-diurnal type same as tides and nearly reversing type. The flood and ebb currents set north and south with a velocity of about 90-175 cm/sec and 120-225 cm/sec at spring tide and begin 0.2 hours after L.W. and 0.7 hours after H. W., respectively. Non-tidal currents flow southward with 10-20 cm/sec at west side of the stream and northward with 15-20 cm/sec at east side of the stream at Inchon Outer Harbor. The flood volume through the Inchon Outer Harbor fluctuates fortnightly from 590 10$\^$6/㎥ spring tide to 260 $10^6/m^3$ at neap tide and ebb volume changes from 470 $10^6/m^3$ at spring tide to 200 $10^6/m^3$ at neap tide, respectively. The flow area along the channel to the Estuary of Yeomha is controlled by the tidal prism as expressed by $A=1.14{\times}10^{-4}P^{0.966}$

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Coastal Typhoon Deposit in the Hampyung Bay, Southwest Coast of Korea

  • Park, Yong-Ahn
    • Journal of the korean society of oceanography
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    • v.31 no.1
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    • pp.32-36
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    • 1996
  • The oyster shell bed (more than 47 cm thick) atop the Gaipri Point (granite coastal bluff) in the Hampyung Bay, southwest coast of Korea which is a coastal area of southeastern margin of the Yellow Sea basin has been interpreted as unique typhoon deposit formed at about 3610 yr BP or later. The unconformable boundary between the oyster shell bed by typhoon and the granitic soil horizon of the Gaipri Point is 820 cm high above the mean high-tide water level (MHWL). The $^{14}C$ age of the oyster shells is 3610${\pm}$70 yr BP.

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Hindcasting of Storm Surge at Southeast Coast by Typhoon Maemi

  • KAWAI HIROYASU;KIM DO-SAM;KANG YOON-KOO;TOMITA TAKASHI;HIRAISHI TETSUYA
    • 한국해양공학회지
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    • v.19 no.2
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    • pp.12-18
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    • 2005
  • Typhoon Maemi landed on the southeast coast of Korea and caused a severe storm surge in Jinhae Bay and Masan Bay. The tide gage in Masan Port recorded the storm surge of a maximum of more than 2m and the area of more than 700m from the Seo Hang Wharf was flooded by the storm surge. They had not met such an extremely severe storm surge since the opening of the port. Then storm surge was hindcasted with a numerical model. The typhoon pressure was approximated by Myers' empirical model and super gradient wind around the typhoon eye wall was considered in the wind estimation. The land topography surrounding Jinhae Bay and Masan Bay is so complex that the computed wind field was modified with the 3D-MASCON model. The motion of seawater due to the atmospheric forces was simulated using a one-layer model based on non-linear long wave approximation. The Janssen's wave age dependent drag coefficient on the sea surface was calculated in the wave prediction model WAM cycle 4 and the coefficient was inputted to the storm surge model. The result shows that the storm surge hindcasted by the numerical model was in good agreement with the observed one.

Holocene 中期에 있어서 道垈川流域의 堆積 環境 變化 (The Change of the Depositional Environment on Dodaecheon River Basin during the Middle Holocene)

  • 황상일;윤순옥;조화용
    • 대한지리학회지
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    • v.32 no.4
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    • pp.403-420
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    • 1997
  • 道垈川은 牙山灣으로 流入되는 小河川이다. Holocene 中期에 있어서 이 流域盆地의 堆積環境變化를 살펴보기 위하여 boring조사, 硅藻${\cdot}$花粉分析, carbon dating 등을 실시했다. 道垈川 流域의 Holocene 堆積層은 土炭層과 靑灰色 실트層이 互層을 이루고 있으며, 많은 硅藻와 花粉化石을 포함하고 있다. 硅藻와 花粉의 分析 결과에 의하면 靑灰色 실트층이 퇴적될 때는 相對的으로 海進의 경향이 있었고, 土炭層이 퇴적될 때는 相對的인 海面의 安定 내지 海退의 경향이 있었다. 後氷期 海岸線은 약 7,000년 BP 경에 현 도대천 하류부에 도달하였고, 그 후 6,000년 BP 까지 몇 차례 小海進과 海退를 거듯하였다. 약 7,000년 BP 경에 해면(평균고조위)은 약 3m에 이르렀고, 미상승과 하강을 거듭하면서 6,000년 BP 경에 약 5m 까지 上昇하였다. 西海岸에서는 海岸低濕地性 土炭地는 약 7,000년 BP 경에서 3,000년 BP 경까지 주로 형성되었고, 이들의 分布高度는 대부분 현재의 平均海面보다 2~6m 높은 위치에 분포하고 있다. 西海岸 土炭地는 대개 高潮位 海面과 관련된 內灣 鹽生濕地性 土炭地이므로, 潮差가 작은 東海岸의 堤間濕地(swale)에서 형성된 土炭地에 비하여 形成時期가 앞서고 分布高度가 높다.

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남해안 사천시 대포동 일대에 분포하는 고해안 퇴적물의 형성 과정과 형성 시기: 한반도 제4기 후기 지각운동의 양식과 변형률 산출을 위한 연구(II) (The Formative Processes and Ages of Paleo-coastal Sediments in Daepo-dong Sacheon-si in the Southern Coast, South Korea: Evaluation of the Mode and Rate of the Late Quaternary Tectonism (II))

  • 신재열;홍성찬
    • 한국지형학회지
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    • v.25 no.3
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    • pp.57-70
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    • 2018
  • This study restores onshore paleo-shoreline records and establishes the nature and strain rate of neotectonism by investigating the existence and formative age of paleo-coastal sediments emerged around Sacheon-si in the Southern part of the Korean peninsula. As a result, paleo-sand bars representing 5m of the paleo-shoreline from high tide level are formed in Sacheon-si, and the formation age of these is confirmed as MIS 5c at approximately 100,000 year BP through rock surface luminescence dating to rounded gravels in paleo-sand bars. Although it is difficult to establish the uplift rate of crust precisely due to incomplete restoration of sea level records during the last interglacial stage, the uplift rate along the Southern coast of the peninsula was assumed approximately 0.72 lower than the Eastern coast during the late Quaternary in comparison to the 1st marine terrace along the Eastern coast.

방파제 모래치환공사시 부유토사의 거동 특성 (Characteristics of Suspended Solids Movement in the Sand Recalmation of Breakwater)

  • 맹준호;이지왕;김병준;고정용;양권열
    • 환경영향평가
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    • v.9 no.2
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    • pp.127-142
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    • 2000
  • This research was performed for analyzing the transport of suspended solids during the harbor construction. In behalf of the research, we have analyzes the characteristics of suspended solids movement in sand reclamation of breakwater according to age of tide and tidal period at the construction spot of Pusan new harbor. In the process of sand reclamation, soil was dumped by a dumping device which direct soil from the barge to the bottom of the sea. According to the results from this research, suspended solid concentration was very high in the range of 5m from the dumping point right after the dumping. However these suspended solids settled very quickly and the solids concentration was very beyond 10m from the dumping point. It is deduced that the movement of solids dumped from barge has the tendencies as following; 1) Most of the dumped solids precipitated quickly after the dumping 2) The rest of the suspended solids are diffused slowly toward the bottom of the water being figured smoothing curve 3) The diffusion movement of suspended solids tend to proceed toward the shore line in a parallel motion with tidal current at the sea-bottom That is to say, most of the suspended solids precipitated very quickly even though highly concentrated solids produced at the bottom of the solids which did not precipitated spread with the tidal current horizontally along the bottom of the sea.

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