• 한국지역지리학회지
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• 제11권1호
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• pp.101-113
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• 2005

한반도의 남서부에 위치한 호남지방은 수리적, 지리적 요인에 의해 지역에 따라 하계의 강수현상 및 탁월일기의 다소와 그 계절변화가 크다. 본 논문은 AWS 63개 지점을 포함한 호남의 79개 기상관측지점의 하계강수량(1994$\sim$2003)과 그 순변화형(강수특성 표현의 중요한 한 요소임)에 대해 순별 강수량의 다소와 순장수량의 주성분벡터와 진폭계수(Rs)를 이용하여, 호남 각 지역에서의 하계강수량 순변화형을 수량적으로 추출하고, 그 공간스케일의 변동을 규명해, 그에 따른 호남지방의 강수지역 구분을 시도한 것이다. 그 결과 호남지방의 하계강수량 순변화의 전형적 특징은 상위 4개의 순변화형으로 표현되며 그 누적기여율은 78.0%이다. 또한 호남지방의 하계강수량의 순변화형은 A-K형까지 11개가 추출되었고, 강수지역은 18개형 지역으로 구분되었다.

• 자원환경지질
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• 제2권4호
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• pp.73-90
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• 1969

The area studied is a southwestern part of Okcheon geosynclinal zone which streches diagonally across the Korean peninsula in the mid-central parts of South Korea, and is bounded by Charyeong mountain chains in the north and by Sobaek mountain chains in the south. The general trend of the zone is of NE-SW direction known as Sinian direction. Okcheon system of pre-Cambrian age occupies southwestern portion of Okcheon geosynclinal zone, and Choseon and Pyeongan systems of Cambrian to Triassic age in northeastern portion of the zone. It was defined by the writer that the former was called "Okcheon Paleogeosynclinal zone" and the latter "Okcheon Neogeosynclinal zone," although T. Kobayashi named them "Metamorphosed Okcheon zone" and "Non-metamorphosed Okcheon zone" respectively and thought that sedimentary formations in both zones were same in origin and of Paleozonic age, and C.M. Son also described that Okchon system was of post-Choseon (Ordovician) and pre-Kyeongsang (Cretaceous) in age. According to the present study two zones are separated by great fault so that the geology in both zones is not only entirely different in origin and age, but also their geolosical structures are discontinuous. Stratigraphy and structure of Okcheon system are clearly established and defined by the writer and its age is definitely pre-Cambrian. It is clarified by present study that the meta-sediments in and at vicinity of Charyeong mountain chains are correlated to Weonnam series of pre-Cambrian age which occupies and continues from northeast to southwest in and at south of Sobaek mountain chains, and both metasediments constitute basement of Okcheon system. Pyeongan, Daedong and Kyeongsang systems were deposited in few narrow intermontain basins in Okcheon paleogeosynclinal zone after it was emerged at the end of Carboniferous period. Granites of Jurassic and Cretaceous ages and volcanics of Cretaceous age are cropped out in the zone. Jurassic granite is aligned generally with the trend of Okcheon geosynclinal zone, whereas Cretaceous granite lacks of trend in distribution. Many isoclinal folds and thrust faults caused by Taebo orogeny at the end of Jurassic period are also parallel with Sinian directieon and dip steeply to northwest. Charyeong, Noryeong, Sobaek, and Deogyu mountain chains are located in areas of anticlinorium, and Kyongsang system in narrow synclinal zones. Folds in Okcheon neogeosynclinal zone are generally of N 70-80W direction but deviate to Sinian direction at the western parts of the zone. This phenomena is interpreted by the fact that the folds were originated by Songrim disturbance at the end of Triassic period and later partly modified by Taebo orogeny. Thrust faults of Taebo orogeny coentinue from Okcheon paleogeosynclinal zone into neogeosynclinal zone, forming imbricated structure as previously described. Strike-slip faults perpendicular to Sinian direction and shear faults diagonally across it by 55 degrees also prevail in neogeosynclinal zone. It is concluded from viewpoints on geology and geological structure that l)Okchon geosyncline had changed its location and affected by numerous disturbances through geologic time, and 2)mountain chains in the area such as Charyeong, Noryeong, Sobaek, and Deogyu were originated as folded mountains. Differing from others, however, Sobaek range was probably formed at the time of Songrim disturbance and modified later by Taebo orogeny. It is cut by Danyang-Jeomchon fault at the vicinity of Joryeong near Munkyeong village and does not continue to southwest beyond the fault, whereas southwestern portion of erstwhile Sobaek range continues to Taebaek rangd northeastward from Deogyusan passing through Sangju, Yecheon, and Andong. From these evidences, the writer has newly defined the erstwhile Sobaek range in such a way that Sobaek range is restricted only to northeastern portion and Deogyu range is named for the southwestern portion of previous Bobaek range.

• 한국수산과학회지
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• 제31권5호
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• pp.695-706
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• 1998

한국 남$\cdot$서해 및 동중국해 북부 해역에 나타나는 표층수온 전선의 위치, 형태, 시기별 변동상황, 전선형성기구 등을 규명하기 위하여 1991년부터 1996년까지 국립수산진흥원에서 NOAA 화상자료로부터 구한 표면수온분포도와 제주도청 어업지도선 등을 이용하여 월별로 관측한 제주해협 해양관측자료를 이용하여 분석 정리한 결과를 요약하면 다음과 같다. 1. 한국 남$\cdot$서해 및 동중국해 북부 해역에 형성되는 연안형 및 외해형 전선대 양상은 여러 가지 Pattern으로 구분되어 진다. 즉, 1월부터 4월까지 한국 남$\cdot$서 연안역에 나타나는 "L" 자형의 연안형 전선대와 제주도 남서쪽 해역에 북서에서 남동방향으로 길게 형성되는 빗금형 ($\setminus$)의 외해형 전선대가 제주도 서쪽 해역에서 서로 마주치지 않아 "L" 자의 "-"를 비스듬히 세운 형상의 동계형 (ㄴ) 전선대가 형성된다. 그리고 6월부터 8월까지 한국 남$\cdot$서해 연안역에만 전선이 나타나는 "L" 자형의 하계형전선대, 5월과 9월, 10원에 나타나는 한국 남$\cdot$서해의 "L" 자형 연안역 전선대와 제주도 남서해역의 외해형전선대가 제주도 주변에서 서로 마주쳐 "Y" 자가 왼편으로 누운 것과 같은 삼거리 모양의 춘$\cdot$추계형 ($\succ$) 전선대가 형성된다. 또 11월과 12월에 나타나는 한국 남해연안역의 직선형의 연안형 전선대와 제주도 남서해역의 외해형 전선대가 제주도 서쪽에서 마주쳐 "$\angle$" 모양으로 되는 늦가을형으로 대별된다. 2. 전선의 단기변동 경향은 수일 이내에는 그 위치가 크게 이동하지 않고, 또 한국 남해 연안역 전선대보다 제주도 남서해역 전선의 위치 변화가 크다. 한국 남해연안역에는 주년 연안형 전선대가 출현하며 이 전선대는 대체로 동계에 연안역에 가장 접근하고 춘$\cdot$추계에 가장 남쪽으로 이동하는 남북 이동을 하며, 제주도 남서해역 외해형 전선대는 대마난류 분포범위의 계절변화와 같이 동계에는 가장 서쪽에, 춘 추계에는 가장 동쪽에 형성되는 동서방향 이동이 있고 한국 남서해역 연안형 전선대도 주년 나타나지만 3월, 4월, 11월에 가장 약화된다. 3. 제주해협에는 추자도에서 여서도 또는 청산도를 잇는 선 부근에 주년 표층수온 전선이 형성되고, 또 11월$\~$1월을 제외한 시기에 제주도 연안에는 하계에 환(Ring-shaped)의 조석전선이 나타나며 특히 5월과 10월에는 제주도 동쪽과 남쪽에 제주도 연안수와 대마난류수간에 전선이 형성되어 한국 남해의 연안형 전선대와 제주도 남서해역의 외해형 전선대를 연결하고 있다.

• 대한지리학회지
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• 제30권1호
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• pp.35-56
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• 1995

본 논문은 지속적인 서울시의 성장이 그 주변지역의 성장을 수반하면서 서울대도시 권화되어가는 과정을 밝히고 서울대도시권역을 설정한 후, 서울대도시권역 내에서 기능적 특성에 따라 지역을 분류하려는 것이 그 목적이었다. 1990년 시점에서의 서울대도시권역의 경계가 어느 정도 확대되었는가를 측정하기 위하여 도시화 정도를 측정하는 지표와 서울과 의 기능적 연계성을 측정하는 지표를 토대로 하여 그 권역을 설정하였다. 그 결과 서울대도 시권역은 수도권의 거의 전 지역을 포함하고 있는 것으로 나타났다. 또한 서울대도시권역에 포함된 지역들은 서울이 갖고 있는 기능을 일부 분담하면서 기능적인 면에서 특화되거나 전 문화되어 기능적 특성에 따라서 신종주거기능 탁월지역, 제조업기능 탁월지역, 서비스기능 탁월지역, 잠재적 개발가능지역의 4개 그룹으로 지역을 분류할 수 있었다.

• 한국환경과학회지
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• 제24권5호
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• pp.601-613
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• 2015

On the study of the characteristics and life cycle of mesoscale convective band in type of airmass that occurred in the Honam area from June to September for only 4 years in the period of 2009~2012, 10 examples based on the amount of rainfall with AWS 24 hours/60 minutes rainfalls, Mt. Osung radar 1.5 km CAPPI/X-SECT images and KLAPS data for convective band with heavy rainfall event were selected. There were analyzed and classified by using the convective band with heavy rainfall occurred along the convergence line of sea wind in the form of individual multi-cellular cell and moving direction of convective band appeared in a variety of patterns; toward southwestern (2 cases), northeastern (4 cases), congesting (2 cases), and changing its moving direction (2 cases). The case study dated of the 17th Aug. 2012 was chosen and implemented by sequentially different evolution of its shape along the convergence line of sea wind cell and moving direction of convective band as equivalent potential temperatures at the lower layer have increased to the upper layer 500 hPa, that the individual cells were developed vertically and horizontally through their merger, but owing to divergence caused by weakened rainfall and descending air current, the growth of new cell was inhibited resulting in dissipation of convective cells.

• Journal of Ecology and Environment
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• 제34권2호
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• pp.137-147
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• 2011

In 2009, United Nations Educational, Scientific and Cultural Organization (UNESCO) recognized the unique outstanding ecosystem biodiversity and distinct ecocultural values of the Shinan Dadohae Biosphere Reserve in the island region. The Dadohae area, which has been sustainably conserved for scores of years, boasts not only a unique ecosystem, but also has residents with a wide range of traditional ecological knowledge. In terms of understanding the soundness of the ecosystem network known as the landscape system, the recent expansion of environmental development has served to heighten the degree of consideration given not only to biodiversity, which has long been used as an indicator to assess ecosystem soundness, but also to assess cultural diversity. Man has used the surrounding landscape and living organisms as his life resources since the beginning. Moreover, whenever necessary, man has developed new species through cultivation. Biodiversity became a foundation that facilitated establishing cultural diversity such as food and housing. Such ecological knowledge has been conveyed not only to adjacent regions, but also at the international level. The recent rapid changes in the Dadohae area island ecosystem caused by the transformation of fishing grounds by such factors as climate change, excess human activities, and marine pollution, is an epoch event in environmental history that shows that the balance between man and nature has become skewed. Furthermore, this issue has moved beyond the biodiversity and landscape diversity level to become an issue that should be addressed at the cultural diversity level. To this end, the time has come to pay close attention to this issue.

• Parasites, Hosts and Diseases
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• 제49권4호
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• pp.381-384
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• 2011

The first human case with trichinellosis was reported in 1964 in Tibet, China. However, up to the present, the etiological agent of trichinellosis has been unclear. The aim of this study was to identify a Tibet Trichinella isolate at a species level by PCR-based methods. Multiplex PCR revealed amplicon of the expected size (173 bp) for Trichinella spiralis in assays containing larval DNA from Tibet Trichinella isolate from a naturally infected pig. The Tibet Trichinella isolate was also identified by PCR amplification of the 5S ribosomal DNA intergenic spacer region (5S ISR) and mitochondrial largesubunit ribosomal RNA (mt-lsrDNA) gene sequences. The results showed that 2 DNA fragments (749 bp and 445 bp) of the Tibet Trichinella isolate were identical to that of the reference isolates of T. spiralis. The Tibet Trichinella isolate might be classifiable to T. spiralis. This is the first report on T. spiralis in southwestern China.

• 한국환경과학회지
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• 제12권2호
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• pp.133-137
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• 2003

The Yellow River delta is an important region where coastal and newly formed wetlands distribute in north China. Based on satellite remote sensing images and GIS techniques, this paper tends to delineate the dynamic changes of newly formed wetland in the Yellow River mouth from 1986.5 to 1996.10. Our results show that the newly formed wetland increased by 24.9 $\textrm{km}^2$ per year. Before 1990. 1 and it decreased by 2.40 $\textrm{km}^2$ per year after that. The northern and southwestern parts of the Yellow River mouth are main positions of decrease and the southern and the estuary parts are main positions of increase. The advancing rate of river mouth extending into the Bo Sea is decreasing obviously. The reason for that is the decreasing of water and sediments in the Yellow River, which caused by the increasing use of water and soil conservation on upper reach.

• 패션비즈니스
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• 제3권3호
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• pp.49-57
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• 1999

In this study, the researcher studied the historical background and the traditional culture about dress of Bouyei People of Guizhou Province. The resuits of the study ara as follows. 1. Women's dress and adorment can be categorized into three styles. In the Zhenning, Guanling and Puding regions and northwestern areas of Guizhou Province, women usually wear blouses with overlapping necks, batik pleated skirts and long aprons. They also wear embroidered kerchiefs or turbans. In the suburbs of Guiyand City and Southwestern Guizhou Province, women like to wear blouses with buttons arranged diagonally on the front, trousers, blue or black and white check cloth kerchiefs. In the Luoping region, women wear blouses with loose sleeves and buttons arranged diagonally on the front and loose-legged trousers. 2. Men usually wear shirts with buttons down the front or arranged on the front, trousers and calottes. 3. Most of their dress materials are white and coloured handwoven, tie-dyed or batik cloth. The exquisite technique of batik and tie-dyeing has a long history, which began to become prevalent in the Song Dynasty. 4. Now, people use all kinds of techniques to make their dress and adornment, including batik, tie-dyeing, cross-stitch, brocade and embroidery, which reflect their peculiar aesthetic temperament.

• 한국수산과학회지
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• 제18권1호
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• pp.67-73
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• 1985

동지나해${\cdot}$황해의 안강망에 의한 어획통계 자료($1967{\sim}1979$) 및 해양관측 자료를 이용하여 부세의 어획량, 어장의 변동과 수온 구조와의 관계를 조사하였다. 그 결과 부세의 주요 어장은 제주도 남서방해역에 집중하였으며, 주어기는 4월이었다. 또한 CPUE는50kg/haul 이상의 해역이 거의 없어 전반적으로 어장이 좋지 않았으며, 변동계수(C.V.)도 컸다. 특히 주어기인 4월에는 수심 50 m의 $10{\sim}8^{\circ}C$ 등온선역에 어장이 분포하였고, 같은 민어과인 참조기${\cdot}$강달이 등에 비해 냉수측에 분포하였다.