• 한국산업융합학회 논문집
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• 제23권5호
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• pp.717-726
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• 2020

Social costs are increasing in Gangwon-do east coast due to coastal erosion. Long-term coastline change information is essential for analyzing this phenomenon. In this study, aerial photographs immediately after liberation are used for 1950's coastline extraction. The study area is from Sokcho Cheongho beach to Yangyang Seorak beach. The aerial photograph is geometrically corrected using DLT(Direct Linear Transformation) method to extract past coastline and compare it with present data. Coastal erosion and deposition areas are calculated in study area. Artificial structures such as harbors and breakwaters have caused changes in ocean currents and sediments from river estuaries. In most cases, the deposition occurred at the southern area of artificial structures and the erosion occurred on surrounding beaches. Coastline information extracted from past aerial photographs can be useful to provide information on long-term changes.

• 한국농공학회논문집
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• 제58권1호
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• pp.61-71
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• 2016

This study performed the physical and mechanical experiment on the samples of costal marine clays individually collected in western and southern regions to identify the characteristics of western and southern costal marine clay. Based on the experiment result, the characteristics of costal marine clay is identified undrained shear strength. Based on the experiment result on the physical and mechanical characteristics of costal marine clays, the regression is presented that can analyze the mechanical characteristics of undrained shear strength in costal marine clay of Korea, region of Korea and western-southern region. The correlation of uniaxial compressive strength and undrained shear strength was suitable for use of western-southern region correlation equation. The test result of Jeonnam Yeosu area compares with prediction results of previous researchers formula and western-southern region formula. Prediction results appear highest reliability on the 0.827 of coefficient of determination in the prediction results of the western-southern region formula.

• 한국항해학회지
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• 제18권1호
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• pp.23-30
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• 1994

By use of the Climatological Report(1982~1991) and the Marine Casualty Report(1982`1992), marine casualties caused by meteorological factors and climatic characteristics along Korean coast were analysed. Marine casualty by meteorological factors can be classified into three kinds such as collision, aground and sinking. On the whole collision was mainly caused by dense fog and heavy precipitation, and aground and sinking was caused by strong wind and high sea. As results of analysis of the distribution of wind, fog and precipitation at major ports in Korea, climatic characteristics along Korean coast are as follows. in the eastern coast, wind was relatively weak and fog was not so frequently formed, while strong wind blew all the year round and fog appeared from April to August in Ulleung Island. In the southern coast, the wind was strong in both winter and summer, fog formed frequently in late spring through mid-summer and heavy precipitation was in summer. Typhoon affecting Korea was usually passing this area to the East Sea. In the western coast, strong wind was prevailing in winter at southern region and fog was formed very frequently throughout the year.

• 한국패류학회지
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• 제7권1호
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• pp.58-65
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• 1991

A study on the distribution and community structure of the benthic molluscan shells of the southern coastral area in Cheju Island was carried out from August 1990 to July 1991. The benthic molluscan shells collected and identified from 8 stations were composed of 3 classes, 7 orders, 22 families and 59 species. The number of appearance species from station 1 to station 8 were 22, 35, 32, 26, 28, 24, 32 and 31 species respectively. the first dominant species of the upper intertidal zone of the 8 stations were Nodilittorina exigua, those of the middle zones were Monodonta neritoides from st.1 to St.5, but the second dominant species were not uniftom at ach station.

• 상하수도학회지
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• 제22권2호
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• pp.195-203
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• 2008

This study collected the latest 30-year (1976~2005) continuous rainfall data hourly recorded at 61 meterological observatories in Korea. The continuous rainfall data was divided into individual rainfall events. In addition, distribution charts of average intervent times between adjacent rainfall events were created to facilitate the application to the overflow risk-based design of storm-water infiltration basin. This study shows that the one-parameter exponential distribution is suitable for the frequency distribution of the average intervent times for the domestic rainfall data. Distribution charts of the average intervent times were created for 4 hour and 6 hour of storm separation time, respectively. The inland Gyeongsangbuk-do and Western coastal area had relatively longer average intervent times, whereas Southern coastal area and Jeju-do had relatively shorter average intervent times.

• 수산해양기술연구
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• 제17권2호
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• pp.105-108
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• 1981

우리나라 남부해안기후의 특성과 수온과의 관계를 알아보기 위하여 해안지방인 부산, 여수, 목포를 준표준 내륙지방으로 광주와 대구, 인근 해양의 가덕도, 소리도, 홍도의 수온을 선정하여 20년 간(1960~1979)의 관측자료로서 기온, 습도, 강수량을 조사 분석한 결과는 다음과 같다. 1) 해안지방(부산, 여수, 목포)은 해양의 영향으로 내륙지방(대구, 광주)보다 기온의 연교차가 적고 기온이 수온보다 높을 때는 내륙지방이 해안지방의 기온보다 높고, 수온이 기온보다 높을 때는 내륙지방이 해안지방보다 낮다. 2) 수온과 기온의 차에 따라서 내륙지방과 해안지방의 기온차가 결정되며(상관계수 0.9이상) 그 양적 예측도 상관관계식을 활용함으로써 가능하다고 생각된다. 3) 해안지방과 내륙지방의 습도의 차이도 기온의 경우와 비슷하게 나타났으나 목포는 지형적인 영향으로 다른 해안지방과 다르게 나타났다. 4) 수온과 기온의 차이에 따라서 해안지방과 내륙지방의 습도의 차이가 결정된다(상관계수 0.9이상, 목포제외), 그러므로 그 양적 해석도 가능하다. 5) 남해안지방의 강수량은 내륙지방과 그 차이가 뚜렷하게 나타나지는 않았다.

• 자원환경지질
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• 제14권2호
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• pp.77-91
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• 1981

An airborne magnetometer survey was carried out over an offshore area of about $200,000km^2$ from the southeastern, southern and western part of Korea. Detailed magnetic studies on the geological structure of the southern part of above area ($100,000km^2$) was accomplished. Residual aeromagnetic map was made in order to delineate magnetic provinces, magnetic lineaments and sedimentary basins by application of least square method using computer system. To determine the depth of the sedimentary basins pseudo-gravimetric method was applied. 1. The area studied is divided into four magnetic provinces for the purpose of interpretation on the basis of the magnetic maps. 2. Near shore area and its attached islands of southern part (fiirst and second magnetic province) can be regarded as being the extension from the land geology due to presentation of strong magnetic anomalies and shallow magnetic basements. 3. Magnetic lineament 1-1 is strong magnetic anomalous region which is presumably relevant to volcanic activities in Cretaceous. The depth of magnetic basement of the lineament was determined to 1,500 m. Negative magnetic anomalous zones B1-1 and B1-2 which represent Tertiary basins showed depth of magnetic basement 3 km and 4 km each. The latter can be interpreted as extension of the Taiwan basin which is consisted of Tertiary sediments. 4. Magnetic lineament 2-1 coincide with Rainan-Fukien massif running NE-SW direction. A lineament located in central part of magnetic lineament 2-1 is well connected with extension of Sobacksan anticlinal axis on land. Volcanic rocks in Gyongsang system concentrated along this lineament. 5. The characteristics of magnetic pattern in the southern Yellow sea basin of western part of Jeju island show weaker magnetic anomalies and deeper magnetic basements than first and second magnetic provinces indicating geological structure of this basin seems to be quite different from that of Jeju strait. 6. In southern part of Jeju island, smoother magnetic pattern develope southward. Maximum depth of magnetic basement in sedimentary basins BIV-1 and BIV-2 were determined down to 6,000 m increasing its thickness toward Taiwan up to 11,000 m in the shelf area off Taichung, Taiwan. Judging from the fact that hydrocarbon was founded in the Tertiary sediments of western coastal area of Taiwan, it can be expected that hydrocarbon will be existed in these sedimentary basins of southern part of Jeju island.

• 한국해안·해양공학회논문집
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• 제34권6호
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• pp.198-210
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• 2022

제주 남부 해협은 대마난류의 분기점으로써 한반도 해역 열염순환의 시작점이 되고 태풍, 쓰나미와 같은 해양 재해의 크기와 빈도에 영향을 미치며 유해생물이나 방사능 오염수가 들어오는 공급원이 되는 등 해양지리학적으로 매우 중요한 영향을 미친다. 따라서 이러한 해상재해 및 재난에 대하여 즉각적인 대응을 위해서는 준 실시간의 해양 관측이 필요하다. 그러나 다른 해협에 비하여 제주 남부의 경우 이러한 해상관측이 부족하며 이로 인해 연구결과 또한 저조한 실정이다. 따라서 본 연구에서는 제주 북부에서의 고주파 레이더 설치 경험을 활용하여 제주 남부에서 레이더 관측에 적합한 지역을 산정하고 고주파 레이더를 설치하여 관측을 진행하였다. 이를 통해 제주 남부해협의 광역 표층해류장을 산출하고 APM(Antenna Pattern Measurement)과 FOL(First Order Line)을 통한 후처리 및 자료 개선을 진행하였으며 이에 대해 실측자료를 활용한 비교분석을 진행하였다. 그 결과 상관계수에서 0.4~0.7, RMSE(Root Mean Square Error) 약 1~19 cm/s의 개선 결과를 보였다. 이러한 고주파레이더 관측결과는 자료 개방 네트워크 구축을 통해 차후에 태풍 대응, 수치모델 검증, 광역 파랑자료의 활용, 해양 수색 구조와 같은 국내 현안 문제를 해결하는데 도움을 줄 것이다.

• 해양환경안전학회지
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• 제15권4호
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• pp.345-354
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• 2009

해역이용협의에 따른 협의서 검토현황과 연안이용형태를 분석한 결과, 공유수면 점 사용은 공작물설치와 해수 취배수, 공유수면 매립은 산업단지조성, 항만 어항개발과 도로건설의 점유율이 높았고, 점 사용은 서해에서 그리고 매립은 남해에서 우세하였다. 지역별로는 전남, 경남지역과 인천 경기지역에서 이용행위가 많았다. 해역이용협의 검토량은 2008년이 전년도에 비해 약 200건 이상 증가하였고, 협의과정에서 준설토 해양투기, 매립, 준설, 해수 취배수, 바다골재채취와 규사채취에 대해 보완요청이 주로 이루어졌다. 연안이용은 대부분 해양환경기준 I등급 또는 II등급의 지역에서 집중되었고, 특히, 법령상 해양 규제지역인 특별관리해역에서는 항만 어항개발과 관련된 매립과 공작물설치, 국립공원에서는 공작물설치와 호안정비가 많았다. 또한, 수산자원보호구역에서는 호안정비, 공작물설치와 해수의 취배수 행위가 많이 이루어진 것으로 평가되었다. 해역이용협의제도의 제반적인 합리성과 신뢰성을 높이는 방법 등 개선방안을 제도운영 및 정책적인 측면과 협의서 작성과 관련한 해양환경영향평가 측면으로 구분해서 정책제언을 제시하였다.

• 대기
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• 제19권2호
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• pp.155-168
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• 2009

Characteristics of seasonal mean diurnal temperature range (DTR) and their causes over South Korea are investigated using the 60 stations data of Korea Meteorological Administration from 1976 to 2005. In general, the seasonal mean DTR is greatest during spring (in inland area) and least during summer (urban and coastal area). The spatial and seasonal variations of DTR are closely linked with the land surface conditions (especially vegetation activity and soil moisture) and atmospheric conditions (cloud amount, precipitation, local circulation). The seasonal mean DTR shows a decreasing trend at the major urban areas and at the north-eastern part of South Korea. Whereas, it shows an increasing trend at the central area of the southern part. Decreasing and increasing trends of DTR are more significant during summer and fall, and during spring and winter. The decrease (increase) of DTR is mainly caused by the stronger increase of daily minimum (maximum) temperature than daily maximum (minimum) temperature. The negative effects of precipitation and cloud amount on the DTR are greater during spring and at the inland area than during winter and at the coastal area. And the effect of daytime precipitation on the DTR is greater than that of nighttime precipitation.