• 제목/요약/키워드: cold water

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The cold water mass along the southeast and east coasts of Korea in 2016-2017

  • Choo, Hyo-Sang
    • Fisheries and Aquatic Sciences
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    • 제24권7호
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    • pp.243-259
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    • 2021
  • The spatial and temporal behaviors and fluctuations of the cold water that appeared in the South East Sea and the East Sea coast from 2016 to 2017 were investigated. The water temperature drop was large in the east coast from April to June and the southeast coast from July to September, and the temperature drop period was longer in the southeast coast. The water temperature fluctuated sensitively to the wind direction, and it gradually decreased in the southwest wind but rose as if jumping in the northeast wind. Wind stress and surface water temperature had an inverse correlation, which was larger in Bukhang-Idukseo, and decreased toward the north of Guryongpo. The cold water appeared mainly in Geojedo-Pohang after 1 to 2 days when the southwest wind was strong, but when the wind became weak, it shrank to the Idukseo (Ulgi-Gampo) and extended into the open sea in a tongue shape. Cold water was distributed only in Samcheok-Toseong in mid-May, Idukseo-Guryongpo and Hupo-Jukbyeon-Samcheok from late May to mid-July, and Bukhang-Idukseo in August-September. The intensity of cold water was greatest in mid-August, and the center of cold water descended from the east coast to the southeast coast from spring to summer. The water temperature fluctuation was dominant at the periods of 1 d and 7-21 d. In wavelet spectrum analysis of water temperature and wind, wind speed increase-water temperature decrease showed phase difference of 12 h in 2 d, 18 h in 3 d, 1.5 d in 4-8 d, and 2-3 d in 8-24 d period. The correlation between the two parameters was large in Geojedo and Namhang, Bukhang-Idukseo, Guryongpo-Jukbyeon, and Samcheok-Toseong. Monitoring stations with high correlation in all periods were generally parallel to the monsoon direction.

소청룡탕(小靑龍湯)의 군신좌사(君臣佐使) 배오(配伍) 분석 (Compatibility Analysis Through the System of Chief, Deputy, Assistant, and Envoy for Socheongnyong-tang)

  • 김도회;윤미정;신순식
    • 대한한의학방제학회지
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    • 제26권4호
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    • pp.363-380
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    • 2018
  • Objectives : We analyzed the principle of compatibility of socheongnyong-tang and expanded the range of application in clinical practice. Methods : Socheongnyong-tang was analyzed by the compatibility principle through the system of chief, deputy, assistant, and envoy, but the basic formulas of "Discussion of Cold Damage" and "Synopsis of the Golden Chamber" was used. Results : Socheongnyong-tang treats exterior wind-cold and interior water accumulation. Exterior wind-cold is treated mainly by exterior-releasing herbs constituting mahwang-tang and gyeji-tang in "Discussion of Cold Damage", and interior water accumulation is treated mainly by retained fluid-resolving herbs constituting yeonggamomigangsinha-tang, yeonggamomigagangsinbanhahaengin-tang and yeonggamomigagangsinbanhaengdaehwang-tang in "Synopsis of the Golden Chamber". Depending on the weight of exterior wind-cold and interior water accumulation, the disease condition is classified as a case where exterior wind-cold is heavier than interior water accumulation, a case where exterior wind-cold is lighter than interior water accumulation, and a case where it is equivalent. When exterior wind-cold is heavier than interior water accumulation, chief herbs are Ephedrae Herba and Cinnamomi Ramulus of exterior-releasing herbs series and deputy herbs are Zingiberis Rhizoma and Asari Radix et Rhizoma of retained fluid-resolving herbs series. When exterior wind-cold is equal to the disease condition of interior water accumulation, chief herbs are Ephedrae Herba of exterior-releasing herbs series and Zingiberis Rhizoma of retained fluid-resolving herbs series, and deputy herbs are Cinnamomi Ramulus of the exterior-releasing herbs series and Asari Radix et Rhizoma of retained fluid-resolving herbs series. When exterior wind-cold is lighter than interior water accumulation, chief herbs are Zingiberis Rhizoma and Asari Radix et Rhizoma of retained fluid-resolving herbs series and deputy herbs are Ephedrae Herba and Cinnamomi Ramulus of exterior-releasing herbs series. In any case, assistant herbs are Pinelliae Rhizoma, Paeoniae Radix alba, and Schisandrae Fructus, and envoy herb is Glycyrrhizae Radix preparata. Conclusions : In conclusion, socheongnyong-tang must differently formulate the system of chief, deputy, assistant, and envoy according to the grade of exterior wind-cold and interior water accumulation. These results suggest that socheongnyong-tang can be applied flexibly when applied in clinical practice to enhance the therapeutic effect.

Monthly Variation of Water Mass Distribution and Current in the Cheju Strait

  • Pang, Ig-Chan;Hong, Chang-Su;Chang, Kyung-Il;Lee, Jae-Chul;Klm, Jun-Teck
    • Journal of the korean society of oceanography
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    • 제38권3호
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    • pp.87-100
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    • 2003
  • The monthly observations of hydrography in the Cheju Strait from September 1995 to June 1998 show that the Cheju Strait is occupied mostly by Tsushima Current Water in winter and coastal waters in summer. In summer, the Yangtze Coastal Water appears in the upper layer and cold water in the lower layer. Especially, the Yellow Sea Bottom Cold Water appears in August 1997, and the clockwise flow of warm water along the northwestern coasts of Cheju Island is disturbed by an eastward expansion of the cold water from the northwest. The cold water expansion seems to be partly associated with strong southeasterly winds. Current measurements in the Cheju Strait suggest that there exists steady eastward barotropic component of about 5 cm/sec, which corresponds to 0.2 Sv barotropic transport in the Cheju Strait. Geostropic transport (baroclinic component) ranges from 0.1 Sv in winter to 0.4 Sv in summer. By adding the barotrophic component of 0.2 Sv, the total transport varies from 0.3 Sv to 0.6 Sv, which is consistent with previous estimations. The transport increase in summer seems to be caused by the expansion of coastal water to the Cheju Strait.

북서태평양에서 난수성(Pleuromamma sp.)과 냉수성(Neocalanus plumchrus) 요각류의 지방 함량 및 구성 분석을 통한 생리/생태 비교 (The Physiological and Ecological Comparisons between Warm (Pleuromamma sp.) and Cold Water Copepod Species (Neocalanus plumchrus) in the Northwestern Pacific Ocean Using Lipid Contents and Compositions)

  • 고아라;주세종;이창래
    • Ocean and Polar Research
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    • 제31권1호
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    • pp.121-131
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    • 2009
  • In an effort to better understand the physiological and ecological differences between warm and cold water copepod species in Korean waters using lipid contents and compositions, two species of copepods (Pleuromamma sp. as a warm water species and Neocalanus plumchrus as a cold water species) were collected from the Northwest Pacific and East Sea/Sea of Japan, respectively. The cold water species showed two fold higher lipid contents than the warm water species (11% vs. 5% of dry weight). Wax esters, known as one of the major storage lipid classes, were found to be the dominant lipid class (accounting for 64% of total lipids) in the cold water species, whereas, in the warm water species, phospholipids, which are known as membrane components, were the dominant lipid class (accounting for 43% of total lipids),with a trace amount of the storage lipids as a form of triacylglycerols (${\leq}1%$ of total lipids). With regard to the fatty acid compositions, saturated fatty acids (SAFA), especially 16:0 (about 30% of total fatty acids), were most abundant in the warm water species, whereas the polyunsaturated fatty acids (PUFA), particularly eicosapentaenoic acid (EPA : 20:5(n-3)) (${\geq}16%$ of total fatty acids), were most abundant in the cold water species. Among the neutral fraction of lipids, phytol, originating from the side chain of chlorophyll and indicative of active feeding on phytoplankton, was detected only in the warm water species. Significant quantities of fatty alcohols were detected in cold water species, particularly long-chain monounsaturated fatty alcohols (i.e. 20:1(n-9) and 22:1(n-11)), which are well known to abound in cold water herbivorous copepods. However, only trace amounts of short-chain fatty alcohols were detected in the warm water species. Twelve different kinds of sterols were detected in these copepod species, with cholest-5-en-$3{\beta}$-ol (cholesterol) and cholesta-5, 24-dien-$3{\beta}$-ol (desmosterol) dominating in cold and warm water species, respectively. In addition, for the warm water species (Pleuromamma sp.), we assessed the latitudinal gradients of lipid contents and compositions using samples from three different latitudinal regions (Philippine EEZ, Japan EEZ, and the East China Sea). Although no latitudinal gradients of lipid contents were detected, the lipid compositions, particularly dietary fatty acid markers, varied significantly with the latitude. The findings of this study confirm that the distribution of lipid contents and compositions in copepods may not only indicate their nutritional condition and diet history, but may also provide insights into their living strategies under different environmental conditions (i.e., water temperature, food availability).

한국 남서연안해역의 저수온 출현과 안개 형성과의 관련성에 관한 연구 (A Study on Relationship between Cold Water Appearance and Fog Formation in the Southwest Coastal Waters of Korea)

  • 윤종휘;정희동;조규대;김동선;이은방
    • 한국항해항만학회지
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    • 제29권6호
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    • pp.583-588
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    • 2005
  • 하계 한국 남서연안 해역에는 저온수가 나타나고 안개가 자주 형성되는 것으로 알려져 있다. 본 연구에서는 저온수의 출현시기 및 장소와 이 해역에서 형성되는 안개에 미치는 저온수의 영향에 대해 조사${\cdot}$분석하였다. 그 결과, 저수온역은 초여름 대흑산도 부근해역에서 나타나기 시작하여, 이것은 점차 이동하여 7월 말${\~}$8월 초 진도 남서쪽 해역에 위치하고, 그 후 10월 중순경 이 해역에서 소멸된다. 그리고 이 해역에서는 주로 4${\~}$8월에 안개가 발생하는데, 특히 인근해역에 비해 해면온도가 현저하게 낮은 진도해역에서 안개 발생빈도가 높은 것으로 보아, 이 해역에 나타나는 저온수가 안개의 형성에 상당한 영향을 끼치는 것으로 사료된다.

위성자료를 이용한 동해안 냉수대의 시공간적 변화 분석 연구 (Study on the temporal and spatial variation in cold water zone in the East Sea using satellite data)

  • 윤석;양현
    • 대한원격탐사학회지
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    • 제32권6호
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    • pp.703-719
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    • 2016
  • 이 연구는 여름철 동해안 냉수대의 시공간적 이동에 따른 변화 분석에 관한 것이다. 2013년 여름에 위성 및 현장자료(바람, 기온, 수온)를 이용하여 다양한 환경 요인들에 기반을 둔 자료 분석을 시도하였다. 냉수대의 생성과 소멸의 영상을 분석하기 위해 AVISO 지형류 및 하루 동안의 천리안 해양관측위성(Geostationary Ocean Color Imager; GOCI) 엽력소 농도 자료를 사용하였다. 또한, 냉수대의 이동을 추적하기 위해 Advanced Very High Resolution Radiometer-Sea Surface Temperature (AVHRR-SST) 자료를 사용하였다. 초여름에 냉수대가 발현하여 늦여름에 소멸한다는 것과 이 기간 동안 냉수대의 생성과 소멸이 지속적으로 반복되었다는 것을 확인할 수 있었다. 추가적으로 냉수대의 후속 영향으로 인해 늦여름에 엽력소 농도가 증가되었다는 것을 확인할 수 있었다.

한국 동해안에 출현하는 냉수괴의 특성과 기원 (CHARACTERISTICS AND ORIGIN OF THE COLD WATER MASS ALONG THE EAST COAST OF KOREA)

  • 김철호;김구
    • 한국해양학회지
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    • 제18권1호
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    • pp.73-83
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    • 1983
  • 동해안에 출현하는 냉수괴의 특성과 기원을 규명하기 위하여 해수의 물리적 특성을 검토하였다. 동해 서남 해역에서 북한 한류계수는 동한난류계수와 만나 전선을 형성하며, 난류계수의 밑으로 침강하여 동해고유수의 위에 위치한다. 침강한 북한 한류계수의 염분은 낮고 용존산소량은 매우 높아 동해고유수와 구별 이 가능함이 발견되었고, 이와 같은 염분과 용존산소의 특성치로써 하계 죽변-축산 연안 해역의 냉수괴는 용승한 동해고유수가 아니라 남하한 북한 한류계수임이 밝혀 졌다. 북한 한류계수는 동계보다 하계에 우세하게 남하하며 남하 하한은 축산-장기갑 해역으로 보인다. 국립수산진흥원이 정밀관측을 실시한 1973년에는 이보다 남쪽인감포 해역에서도 북한 한류계수의 특성이 발견되었다.

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Study On The Coastal Cold Water Near Ulsan

  • Lee, Ki-Baik
    • 한국해양학회지
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    • 제13권2호
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    • pp.5-10
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    • 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.

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Study on the Anthropometric and Body Composition Indices for Prediction of Cold and Heat Pattern

  • Mun, Sujeong;Park, Kihyun;Lee, Siwoo
    • 대한한의학회지
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    • 제42권4호
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    • pp.185-196
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    • 2021
  • Objectives: Many symptoms of cold and heat patterns are related to the thermoregulation of the body. Thus, we aimed to study the association of cold and heat patterns with anthropometry/body composition. Methods: The cold and heat patterns of 2000 individuals aged 30-55 years were evaluated using a self-administered questionnaire. Results: Among the anthropometric and body composition variables, body mass index (-0.37, 0.39) and fat mass index (-0.35, 0.38) had the highest correlation coefficients with the cold and heat pattern scores after adjustment for age and sex in the cold-heat group, while the correlation coefficients were relatively lower in the non-cold-heat group. In the cold-heat group, the most parsimonious model for the cold pattern with the variables selected by the best subset method and Lasso included sex, body mass index, waist-hip ratio, and extracellular water/total body water (adjusted R2 = 0.324), and the model for heat pattern additionally included age (adjusted R2 = 0.292). Conclusions: The variables related to obesity and water balance were the most useful for predicting cold and heat patterns. Further studies are required to improve the performance of prediction models.

2019년 여름철 제주해협에서 관측된 중층 저온수의 분포와 기원 (Distribution and Origin of the Mid-depth Cold Water Pools Observed in the Jeju Strait in the Summer of 2019)

  • 유도협;김종규;최병주
    • 한국해양학회지:바다
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    • 제28권1호
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    • pp.19-40
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    • 2023
  • 여름철 제주해협 물성 분포의 특성과 제주해협 수괴가 연안에 미치는 영향을 확인하기 위하여 2019년 6월, 7월, 8월에 완도와 제주도 사이에서 수온과 염분을 관측하였다. 여름철 계절 수온약층 아래에서 15℃의 저온수가 관측되었으며, 이 저온수는 관측시기에 따라 다르지만 수심이 깊은 제주해협 남쪽 골보다는 주로 제주해협 중앙의 중층과 북쪽 사면에 분포하였다. 이 저온수를 구성하는 근원 수괴를 알아보기 위하여 제주해협에서 관측된 해수를 구성하는 주변 근원 수괴들의 혼합비(mixing ratio)를 계산하였다. 여름철 제주해협 중앙 중층과 북쪽 사면에 나타나는 저온수는 평균적으로 쿠로시오 아표층수가 54% 그리고 황해저층냉수가 33% 비율로 혼합된 해수였다. 이 중층 저온수는 제주해협 전 수층에서 가장 낮은 수온을 갖는 해수임에도 상대적으로 고온고염인 쿠로시오아표층수가 큰 구성비율을 갖고 있다. 중층 저온수가 제주해협에서 가장 낮은 수온의 분포를 갖게 된 이유는 다른 제주해협 해수에 비해 황해저층냉수의 기여도가 높기 때문이다. 제주해협 중층 저온수의 기원을 살펴보기 위하여 황해, 동중국해, 대한해협에서 2019년 여름철에 관측한 광역 수온과 염분 자료를 분석하였다. 제주도 남서쪽 동중국해 계절 수온약층 아래에서 쿠로시오 기원의 해수와 황해저층냉수가 열염전선을 형성하였고, 이 열염전선을 가로지르는 수괴의 관입에 의해 해수의 혼합이 발생하였다. 동중국해에서 형성된 이 혼합수는 제주해협에서 관측된 중층 저온수와 거의 같은 혼합비율을 가졌다. 이런 결과들을 종합하였을 때 제주해협에서 여름철에 관측된 중층 저온수는 동중국해에서 쿠로시오 아표층수와 황해저층냉수의 혼합으로 만들어진 저온수가 해류를 따라 이동한 것이다. 제주해협 중앙과 북쪽 사면으로 이동한 중층 저온수는 제주해협 중앙의 중층에서 수온역전을 만들고, 한국 남해안 연안의 표층 수온 변동에도 큰 영향을 미친다.