• Title/Summary/Keyword: The East Coast

Search Result 1,159, Processing Time 0.028 seconds

A Political-Economic Study on Cooperative Squid Fishing East to the $E128^{\circ}$ (동경 128도 이동 오징어 공조조업에 관한 정치경제학적 연구)

  • Park Seong-Kwae
    • The Journal of Fisheries Business Administration
    • /
    • v.35 no.2
    • /
    • pp.91-115
    • /
    • 2004
  • The main purpose of this study is to analyze the cooperative squid fisheries problems surrounding the $E128^{\circ}$, established by the 1965 Korea - Japan Fisheries Agreement which banned Korean large trawlers' fishing east to the $E128^{\circ}$ In fact, the moratorium was put on by Japans request. However, such issue did not occur until the filefish stock in the southern Korean sea, which was a major target fish species of the large trawl fisheries, The filefish stock collapsed completely around 1991 and at the same time most of bottom fish stocks in the East China Sea began to show a symptom of over - exploitation. Thus, the off - shore large trawlers learned to have a little opportunity of finding out alternative fish stocks as well as fishing grounds. Fortunately, at that time squid resource stock and consumption were on the increasing trend. The large trawl fisheries were able to economically exploit squid stock east to the $E128^{\circ}$ through cooperative fishing with squid angling light boats in the East and East - South Sea, even though such cooperative fishing activities violate the existing fishery laws apparently. Some important reasons that the large trawlers have continued the cooperative fishing seem to be because (ⅰ) squid resource stock has been on the increasing state over time, (ⅱ) the trawl fisheries have made a significant contribution to meeting domestic and export demands and stabilizing squid prices, and (ⅲ) they have kept domestic squid market from foreign competition. However, the new Korea - Japan fisheries agreement in 1998 provided a momentum of questioning the effectiveness of the $E128^{\circ}$ by the squid - related fisheries other than the squid angling. Serious conflicts between squid - related fisheries began to emerge and to be much intensified. Squid angling industries in the East opposed to large trawlers's efforts to formalize such illegal cooperative squid fishing activities. Their main argument was that such formalizing would definitely make the East coast squid prices lower and in turn their business performance would be worse off. The results of quantitative analysis suggest that the trawlers' massive landing may have a significant influence on lowering the east coast squid prices. Now, an important issue that the squid - related fisheries and the government are facing is to solve such complex squid fishing problems through a multi - participatory negotiation process, including price stabilization, total allowable catch level and its operation schemes, $E128^{\circ}$ rearrangement, and so on.

  • PDF

Seasonal Variation in Subtidal Seaweed Community Structure at Hajung, on the Southeast Coast of Korea (동해안 남부 하정 연안의 조하대 해조류 군집구조의 계절적 변화)

  • Kim, Young-Dae;Park, Mi-Seon;Yoo, Hyun-Il;Min, Byung-Hwa;Moon, Tae-Seok;Choi, Han-Gil
    • Korean Journal of Fisheries and Aquatic Sciences
    • /
    • v.44 no.6
    • /
    • pp.740-746
    • /
    • 2011
  • Subtidal benthic macroalgal flora and community structure on barren grounds were examined seasonally along vertical shore gradients on the rocky shore of Hajung, Pohang, on the southeast coast of Korea, from February 2005 to November 2006. Twenty-six seaweed species were identified, including 5 green, 7 brown, and 14 red algae. The number of seaweed species ranged between 7 and 17 among seasons and between 13 and 20 species were found in vertical gradients along the shore. Over the study period, average seaweed biomass (g wet wt/$m^2$) was 299.88 g and it ranged seasonally from 120.99 to 620.00 g. Seaweed biomass declined with increasing seawater depth and ranged between 323.06 and 593.68 g. The dominant seaweed species, in terms of biomass, were Desmarestia ligulata and Sargassum honeri, which grew at depths between 5 and 10 m. The red alga Delisea pulchra was also abundant at a depth of 15 m. No seasonal patterns were found in community indices. Along vertical shore gradients, community indices showed different patterns; the dominance index increased and the richness, evenness, and diversity indices decreased with seawater depth.

Geomorphic development and distributional system of marine terrace in the eastern part of Seopo-myeon, Sacheon-si, Gyeongnam Province (경남 사천시 서포면 동쪽 해안단구 지형 발달과 분포 체계)

  • Yoon, Soon-Ock;Kang, Bong;Park, Chung-Sun;Hwang, Sangill
    • Journal of the Korean association of regional geographers
    • /
    • v.22 no.4
    • /
    • pp.875-886
    • /
    • 2016
  • The eastern coast of Seopo-myeon, Sancheon-si in the South Coast is a bay almost completely separated from open sea by Changseon and Namhae Islands. Marine terraces in this area can be classified into geomorphic surfaces with elevations of 10~12m, 15~18m, 20~24m, 25~28m, 30~33m, 35~38m, 40~45m, 45~50m and 54m. This marine terrace system is similar to the Boryeong area in the West Coast. The geomorphic surfaces distribute along ridges and show relatively small areas. The young and old surfaces show a mixed distributional pattern. This distributional pattern contrasts to the East Coast where the oldest surface farthest from the coastline is parallel to the coast and age of the surfaces increases with a distance from the coast. These seem to result in high energy waves by typhoon that developed wave-cut platform on hill areas with relatively complex relief in a short time.

  • PDF

A Numerical Simulation of 1983 East Sea Tsunami (1983년(年) 동해(東海)쓰나미의 산정(算定))

  • Choi, Byung Ho;Lee, Ho Jun
    • KSCE Journal of Civil and Environmental Engineering Research
    • /
    • v.13 no.3
    • /
    • pp.207-219
    • /
    • 1993
  • Tsunamis along the east coast of Korea accompanying the 1983 East Sea central region earthquake is hindcasted with numerical models for tsunami propagation and inundation. Both linear and nonlinear models were used to compute propagation and elevation of tsunami waves on the coastal area of Korea. For the mesh refinement, grid system was divided into two sub-regions in Korean coastal area with final 10m grid resolution at interior area where serious inundation was observed. Calculated tsunami height distribution showed a general agreement with coastal observation. With interior detailed mesh system at mid-east coast region, the inundatin at the port of Imwon were qualitatively well reproduced by inundation and runup model.

  • PDF

Morphometric Analysis of Zostera marina L. Found in Various Habitats Along the Eastern Coast of Korea (동해안에 자생하는 거머리말(Zostera marina L.)의 생육지 분포에 따른 형태 분석)

  • 권천중;이상용;최청일
    • Korean Journal of Environmental Biology
    • /
    • v.20 no.1
    • /
    • pp.66-72
    • /
    • 2002
  • The intraspecific variability, habitats, and morphological characteristics of eelgrass (Zostera marina L.) along the eastern coast of Korea were examined during June to August 1998. Morphological characteristics including shoot height, leaf length, leaf width, number of leaf veins, and shape of leaf apex were measured, and eelgrass habitats were analyzed using character correlation, principal components and cluster analyses. The morphological characteristics varied with the habitat types and water depth. Eelgrass beds distributed mostly in lagoons, ports and bays along the east coast of the Korean peninsula. The quantitative morphological features that enabled recognition of the two phonetic groups were short- narrow and long-broad leaf types. Leaf apex in particular varied with the habitat characteristics.

Study On The Coastal Cold Water Near Ulsan

  • Lee, Ki-Baik
    • 한국해양학회지
    • /
    • v.13 no.2
    • /
    • pp.5-10
    • /
    • 1978
  • The coastal cold water near Ulsan, Korea, almost always appears in summer. From the results of some data analysis, it is found that this cold water has an important relation to the anticlockwise circulation appearing near the coast where the anticlockwise circulation turns its current direction from south to east.

  • PDF