• Title/Summary/Keyword: East Sea coast

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동해안 무속장단 변주유형의 운영 - 굿거리장단을 중심으로 (The performance on East Sea Coast Shamanism Gutguri rhythm's variation types - Centered on Gutguri rhythm)

  • 홍성현
    • 공연문화연구
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    • 제40호
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    • pp.343-372
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    • 2020
  • 본고는 동해안 무속에서 사용하는 굿거리장단의 변주유형의 운영을 연구한 논문이다. 동해안 별신굿 예능보유자였던 고(故)김용택의 굿거리장단 연주가 다른 장르에서 보았던 굿거리장단과 색다르게 다가왔고 그 요인을 찾기 위해 그가 연주할 때 사용하는 변주유형과 연주기법들을 살펴보았다. 동해안 무속 굿거리장단은 여타 다른 장르에서 연주되는 굿거리장단의 유형과 기법보다 다양한 변주유형이 존재하며 독특한 형태의 기법들을 사용하고 있다. 이 같은 다양한 변주유형과 독특한 연주기법이 실제 연주에 반영되어 즉흥적인 변주가 이루어지고 있다.

국내 대표 해양·수산 과학논문 분석을 통한 우리나라 주변 바다 이름표기에 대한 제언 (Nomenclature of the Seas Around the Korean Peninsula Derived From Analyses of Papers in Two Representative Korean Ocean and Fisheries Science Journals: Present Status and Future)

  • 변도성;최병주
    • 한국해양학회지:바다
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    • 제23권3호
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    • pp.125-151
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    • 2018
  • 지난 20년간(1998-2017년) 한국해양학회지(바다)와 한국수산과학회지에 실린 한글 논문 중 우리나라 주변 바다 이름을 지도에 표기한 논문들을 대상으로 그 표기 방법을 살펴보았다. 지도에 표기된 바다 명칭들의 형태는 크게 세 가지 - 'East Sea(동해)와 Yellow Sea(황해)', 'East Sea(동해), Yellow Sea(황해), South Sea(남해)', 'East Sea(동해), West Sea(서해), South Sea(남해)' - 가 있다. 'East Sea'는 모든 논문에서 'East Sea'로 표기된 반면, 'Yellow Sea'는 'West Sea'와 혼용해서 사용되고 있었다. 'Korea Strait(대한해협)' 대신 'South Sea'의 사용 빈도도 높았다. 이 결과는 연구자들이 해안선으로부터 가까운 연안해역을 우리나라를 기준으로 지리적 방위에 근간하여 부를 때 사용하는 바다 명칭과 주변해에 대한 국제적인 바다 명칭을 혼용하여 사용하고 있음을 보여 준다. 따라서 우리나라 해양 수산 연구자들이 바다 이름표기에 관한 기준을 세우고 일관성 있게 표기하는 것이 시급하다. 이와 관련하여 이 연구에서는 연구논문 작성 시에 주변해와 우리나라 연안해역에 대한 바다 명칭을 서로 구분하여 사용할 것을 제안하였다. 즉, 주변해는 국제적으로 통용되고 있는 'East Sea(동해)', 'Yellow Sea(황해)', 'Korea Strait(대한해협)', 'East China Sea(동중국해)'로 사용하고, 이들 주변 바다에 포함되어 있는 연안해역은 우리나라를 기준으로 상대적 방위에 근거한 'Coastal Sea off the East Coast of Korea(한국 동쪽 연안 바다)', 'Coastal Sea off the West Coast of Korea(한국 서쪽 연안 바다)', 'Coastal Sea off the South Coast of Korea(한국 남쪽 연안 바다)' 등으로 표현할 수 있다. 다른 표현으로는 'East Korea Coastal Zone', 'South Coastal Zone of Korea', 'West Korea Coastal Zone'으로도 표현할 수 있다. 작은 규모의 특정 해역의 경우 해양지명(해상지명과 해저지명)을 사용하여 연구해역을 표기할 수 있다.

Boussinesq 방정식을 이용한 동해지진해일 수치실험 연구 (A Study on the Numerical Simulation of the Seismic Sea Waves in the East Sea based on the Boussinesq Equation)

  • 김성대;정경태;박수영
    • Ocean and Polar Research
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    • 제29권1호
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    • pp.9-31
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    • 2007
  • Most seismic sea waves in the East Sea originate from earthquakes occurring near the Japanese west coast. While the waves propagate in the East Sea, they are deformed by refraction, diffraction and scattering. Though the Boussinesq equation is most applicable for such wave phenomena, it was not used in numerical modelling of seismic sea waves in the East Sea. To examine characteristics of seismic sea waves in the East Sea, numerical models based on the Boussinesq equation are established and used to simulate recent tsunamis. By considering Ursell parameter and Kajiura parameter, it is proved that Boussinesq equation is a proper equation for seismic sea waves in the East Sea. Two models based on the Boussinesq equation and linear wave equation are executed with the same initial conditions and grid size ($1min{\times}1min$), and the results are compared in various respects. The Boussinesq equation model produced better results than the linear model in respect to wave propagation and concentration of wave energy. It is also certified that the Boussinesq equation model can be used for operational purpose if it is optimized. Another Boussinesq equation model whose grid size is $40sec{\times}30sec$ is set up to simulate the 1983 and 1993 tsunamis. As the result of simulation, new propagation charts of 2 seismic sea waves focused on the Korean east coast are proposed. Even though the 1983 and 1993 tsunamis started at different areas, the propagation paths near the Korean east coast are similar and they can be distinguished into 4 paths. Among these, total energy and propagating time of the waves passing over North Korea Plateau(NKP) and South Korea Plateau(SKP) determine wave height at the Korean east coast. In case of the 1993 tsunami, the wave passing over NKP has more energy than the wave over SKP. In case of the 1983 tsunami, the huge energy of the wave passing over SKP brought about great maximum wave heights at Mukho and Imwon. The Boussinesq equation model established in this study is more useful for simulation of seismic sea waves near the Korean east coast than it is the Japanese coast. To improve understanding of seismic sea waves in shallow water, a coastal area model based on the Boussinesq equation is also required.

동해안 해안선과 해빈의 계절적 변화 (Seasonal Changes of Shorelines and Beaches on East Sea Coast, South Korea)

  • 김대식;이광률
    • 대한지리학회지
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    • 제50권2호
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    • pp.147-164
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    • 2015
  • 본 연구는 동해안의 8개 해빈을 대상으로 2012년 3월부터 2014년 2월까지 2년 동안 지형 측량을 실시하여, 해안선과 해빈의 계절적 변화 특성과 경향을 파악하였다. 동해안의 해안선은 계절적 변화량이 연간 변화량보다 크게 나타났고, 강원도와 경상북도 해안의 계절적 변화 양상에는 지역적인 차이가 다소 존재하였다. 동해안 8개 해빈의 계절적 변화를 종합하면, 여름철에는 해안선의 후퇴와 해빈의 침식이, 가을철에는 해안선의 전진과 해빈의 퇴적이 뚜렷하게 나타났다. 이러한 결과는 세계의 여러 중위도 해안의 계절적 변화 경향과는 다르지만, 우리나라 서해안 및 동해안의 선행 연구와는 대체로 일치한다. 여름철에 우세하게 발생하는 침식 현상은 태풍에 의한 폭풍파가 가장 큰 요인이며, 폭풍파에 의한 해안 침식은 늦겨울에도 잘 나타난다. 그리고 가을철에 우세한 해빈의 퇴적 현상은 여름철의 강한 침식 이후에 발생하는 해안 평형 작용의 결과로 판단된다.

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Comparison of RIAMOM and MOM in Modeling the East Sea/Japan Sea Circulation

  • Lee, Ho-Jin;Yoon, Jong-Hwan;Kawamura, Hideyuki;Kang, Hyoun-Woo
    • Ocean and Polar Research
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    • 제25권3호
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    • pp.287-302
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    • 2003
  • The seasonal variations in the circulation of the water mass in the East Sea/Japan Sea have been simulated using a free surface primitive ocean model, RIAMOM (RIAM Ocean Model), comparing the results from GFDL-MOM1 (Geophysical Fluid Dynamics Laboratory Modular Ocean Model, version 1.1, hereafter MOM) with the GDEM (Generalized Digital Environmental Model) data. Both models appear to successfully reproduce the distinct features of circulation in the East Sea/Japan Sea, such as the NB (Nearshore Branch) flowing along the Japanese coast, the EKWC (East Korean Warm Current) flowing northward along the Korean coast, and the NKCC/LCC (North Korean Cold Current/Liman Cold Current) flowing southwestward along Korean/Russian coast. RIAMOM has shown better performance, compared to MOM, in terms of the realistic simulation of the flow field in the East Sea/Japan Sea; RIAMOM has produced more rectified flows on the coastal region, for example, the narrower and stronger NKCC/LCC than MOM has. There is however obvious differences between the model results and the GDEM data in terms of the calculation of the water mass; both models have shown a tendency to overpredict temperature and underpredict salinity below 50m; more diffusive forms of thermocline and halocline have been simulated than noted in GDEM data.

Fluctuations of Coastal Water Temperatures Along Korean and Japanese Coasts in the East Sea

  • KANG Yong-Q.;CHOI Seong-Won
    • 한국수산과학회지
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    • 제21권6호
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    • pp.351-360
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    • 1988
  • Based on historic data of monthly means of sea surface temperatures (SST) for 24 years $(1921\~1944) $ at 23 Korean and Japanese coastal stations in the East Sea (the Japan Sea), we analyzed spatio-temporal characteristics of coastal SST and SST anomalies. The means of SST at Korean coast are higher than those at Japanese coast of the same latitudes, and the annual range of SST at Korean coast are larger than those at Japanese coast. Empirical orthogonal function analysis shows that almost all $(96\%)$ of the SST fluctuations are described by simultaneous seasonal variations. The flurtuations of SST anomalies are small in the Korea Strait and large at the boundaries between the warm and told currents in the basin. The fluctuations of SST anomalies along Korean coast are correlated each other The same is true for SST anomalies along Japanese coast. However, there is only weak correlation between the SST anomalies at Korean coast and those at Japanese coast. Empirical orthogonal function analysis shows that $27\%$ of the coastal SST anomalies in the East Sea are described by simultaneous fluctuations, and $12\%$ of them are described by alternating fluctuations between Korean and Japanese coasts.

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Variation of the Sea Level in the Korean seas Using Altimeter Data (TOPEX/POSEIDON)

  • Seo, Won-Chan;Yoon, Hong-Joo
    • Journal of information and communication convergence engineering
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    • 제6권4호
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    • pp.430-433
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    • 2008
  • A merged altimeter data products are used to estimate sea level variation in the East Sea between 1993 and 2006. The altimeter data show a high correlation coefficient (0.85) after applying gaussian low pass filter for 180days at Ulleung island. The both of Mukho coast and Ulleung island are minimal sea level in March to May and maximal in September to November. Sea level of Mukho coast is higher than that of Ulleung island during March to May, while Mukho coast is lower during September to November because the North Korea Cold Current flows along the coast line of Mukho. Generally sea level variation at Mukho coast and Ulleung island associated with seasonal variations.

개별여행비용법(TCM)을 이용한 동해안 해수욕장의 경제적 가치추정 (Estimating the Economic Value of the East Sea Beach Using Individual Travel Cost Method)

  • 표희동
    • Ocean and Polar Research
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    • 제39권1호
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    • pp.51-59
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    • 2017
  • The purpose of this paper is to estimate the economic value of beaches which are the major part of the East Sea Coast. ITCM (Individual Travel Cost Method) is applied to estimate the economic value of its beaches using Poisson, negative binomial, truncated Poisson and truncated negative binomial models. The consumer surplus during length of stay per capita is 214,088 won in beaches overall on the East Sea Coast, 206,398 won in Gangwon-do beaches and 271,171 won in Gyeongbuk/Ulsan beaches. Annual total economic value of its beaches considering the number of visitors at beaches is 6,269 billion won (3,970 billion won in Kangwondo beaches, 2,299 billion won in Kyungbuk/Ulsan beaches).

해안가의 계절별 비래염분량의 분포 특성 (Distribution properties of seasonal airborne sea salt in the seashore)

  • 이종석;최원성;문한영
    • 한국콘크리트학회:학술대회논문집
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    • 한국콘크리트학회 2004년도 추계 학술발표회 제16권2호
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    • pp.237-240
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    • 2004
  • When the concrete structures are in contact with seawater, concentration of chloride for estimating chloride diffusion coefficient can be defined as the chloride concentration of sea water. However, in case the concrete structures, constructed in the seashore, aren't directly in contact with seawater, it is difficult to establish the interface concentration of chloride. In addition, marine concrete structures are greatly affected by salt attack such as rebar corrosion, among the cause of salt attack, airborne sea salt is primary factor. Therefore, in this study, salt attack environment by airborne sea salt was investigated in terms of a seasonal distribution at 33 spots, 6 areas in the East, West, South coast for 1 year. Results indicated that in the South coast, the amount of the airborne sea salt is comparatively higher in summer. in the West coast. higher in winter. On the other hand, in the East coast, the amount of the airborne sea salt is rarely affected by a season.

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동해와 남해 연안에 서식하는 군소(Aplysia kurodai) 서식지 주변의 해조상과 위 내용물 조성 (Composition of the Stomach Contents and Marine Algal Flora Around Sea Hare Aplysia kurodai Habitats in the East and South Coast of Korea)

  • 김민주;김남길
    • 한국수산과학회지
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    • 제56권1호
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    • pp.66-78
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    • 2023
  • The sea hare Aplysia kurodai is an economic species located along the Korean coast. This study aimed to investigate the stomach contents of A. kurodai and its relationship with marine algal flora surrounding their habitat. A. kurodai and marine algae were sampled in seven and five areas in the East and the South seas, respectively. The marine algae found in the stomach and surrounding marine habitat were identified. In the East Sea of Korea, 134 species of seaweed were recorded. Thirty-nine species of marine algae were identified in the stomach contents of A. korudai collected from the East Sea of Korea. Seventy-five species of seaweed were collected in the South Sea of Korea. In addition, 26 species of marine algae were identified in the stomach contents of A. kurodai from the South Sea of Korea. Among the stomach contents of A. kurodai, ten sheet,12 filamentous, 27 coarsely branched, and one jointed calcareous form species were identified.