• 한국지구과학회지
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• 제43권6호
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• pp.712-736
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• 2022

To understand the characteristics of low-level clouds (CLs), environmental variables are composited on each CL using individual surface observations and six-hourly upper-air meteorologies around the globe. Individual CLs has its own distinct environmental conditions. Over the eastern subtropical and western North Pacific Ocean in JJA, stratocumulus (CL5) has a colder sea surface temperature (SST), stronger and lower inversion, and more low-level cloud amount (LCA) than the climatology whereas cumulus (CL12) has the opposite characteristics. Over the eastern subtropical Pacific, CL5 and CL12 are influenced by cold and warm advection within the PBL, respectively but have similar cold advection over the western North Pacific. This indicates that the fundamental physical process distinguishing CL5 and CL12 is not the horizontal temperature advection but the interaction with the underlying sea surface, i.e., the deepening-decoupling of PBL and the positive feedback between shortwave radiation and SST. Over the western North Pacific during JJA, sky-obscuring fog (CL11), no low-level cloud (CL0), and fair weather stratus (CL6) are associated with anomalous warm advection, surface-based inversion, mean upward flow, and moist mid-troposphere with the strongest anomalies for CL11 followed by CL0. Over the western North Pacific during DJF, bad weather stratus (CL7) occurs in the warm front of the extratropical cyclone with anomalous upward flow while cumulonimbus (CL39) occurs on the rear side of the cold front with anomalous downward flow. Over the tropical oceans, CL7 has strong positive (negative) anomalies of temperature in the upper troposphere (PBL), relative humidity, and surface wind speed in association with the mesoscale convective system while CL12 has the opposite anomalies and CL39 is in between.

• 대한기계학회논문집B
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• 제24권9호
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• pp.1264-1276
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• 2000

Light-off catalyst has been used for minimization of cold-start emissions. Improved cold-start performance of light-off catalyst needs the optimal design in terms of flow distribution, geometric surface area, precious metal loading, cell density and space velocity. In this study, these influential factors are numerically investigated using integrated numerical technique by considering not only 3-D fluid flow but also heat and mass transfer with chemical reactions. The present results indicate that uneven catalyst loading of depositing high active catalyst at upstream of monolith is beneficial during warm-up period but its effect is severely deteriorated when the space velocity is above 100,000 $hr^{-1}$ To maximize light-off performance, this study suggests that 1) a light-off catalyst be designed double substrate type; 2) the substrate with high GSA and high PM loading at face be placed at the front monolith; and 3) the cell density of the rear monolith be lower to reduce the pressure drop.

• 한국기계가공학회지
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• 제19권9호
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• pp.93-99
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• 2020

Recently, as the weight reduction of vehicles has been actively progressed, parts developed using aluminum 60XX series from existing steel materials are increasing. In this paper, the bushing used for the front frame rail, which is one of the parts for fixing engines and other parts in automobiles, was changed to an aluminum material of the Al60XX series, and it was intended to be produced by applying of cold forging method. The bushing is a part that secures the engine frame, and in order to produce it by cold forging, the molding limit is predicted through process design, and a multi-stage process is designed through finite element analysis. In addition, in order to verify the feasibility of the designed forging process, the limits of the multi-step process were verified based on the Cockcroft Latham theory, and the crack and overlap of the actual forging work were predicted and improved.

• Ocean and Polar Research
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• 제26권4호
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• pp.595-606
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• 2004

Hydrographic survey in the Korea Strait has long history that has begun in August 1917 at the Busan - Tsushima cross section, still continues to date. However, chemical properties of bottom cold water found exclusively in the western channel of the Korea Strait during summer did not receive much scientific attention. The aim of the study is to decipher the enigmatic origin of the Korea Strait Bottom Cold Water (KSBCW) in terms of chemical properties. The physicochemical properties of the KSBCW are extracted from the CREAHS II hydrographic data. OMP method was applied to analyze origin of the KSBCW quantitatively. The KSBCW is well defined by low temperature below $10^{\circ}C$. The cold waters exhibited the local presence near the coast at about 120m depth with a thickness of 20m to 30m. The cold water was characterized by relatively cold, saline and higher chemical concentrations than adjacent waters. The KSBCW seems to have different origin kom that of the coastal upwelled waters at the Ulgi-Gampo because it is saline, denser and contains considerably less dissolved oxygen than upwelled waters. The physicochemical properties are reported to have noticeable annual variations which suggest the complex origin of the KSBCW. OMP analysis show that the KSBCW is a mixture of three water types; TMW (24%), ESIW (36%) and ESPW (40%). Relationship between the KSBCW and the east Sea circulation is traced by mapping the water masses that have similar T, S and DO of KSBCW. The result showed that the KSBCW is most possibly an extension of southward flowing coastal intermediate waters. Front these results, we expect that the monitoring KSBCW will provide us valuable information about the East Sea circulation.

• 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.

• Journal of the korean society of oceanography
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• 제37권4호
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• pp.212-223
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• 2002

Cochlodinium polykrikoides bloom in 1995 was studied with a focus on an unusual coastal environment in the South Sea of Korea. Data on temperature, salinity, and zooplankton biomass during 1965-1998 and nutrients during 1990-1998 and chlorophyll-a during 1995-1998 were used in this study. These data were obtained from the serial oceanographic observations in Korean waters carried out by the National Fisheries Research and Development Institute. In 1995 the C. polykrikoides bloom began in the coastal area around Narodo Island in August and consequently occurred to the whole coastal area of the South and East Seas of Korea. During June-October 1995, the coastal environment was unusual compared with the long-term means during 1965-1998. In June 1995, sea surface temperature was 1-2$^{\circ}C$ warmer than in other years in all coastal areas, while salinity was high only to the east of Jeju Island. In August 1995, a strong coastal front appeared inshore of a line between Jeju and Tsushima Islands. In particular, a strong coastal front which showed the characteristics of upwelling front occurred in the coastal area around Narodo and Sorido Islands, not only because of a strong intrusion of the Tsushima Warm Current but also because of the upwelling of cold bottom water. Salinity was low in the neighboring waters of western side of Jeju Island. Nutrients and chlorophyll-a were high in the inshore area between Narodo and Sorido Islands in 1995 in contrast with the other years and areas. Zooplankton showed an unusually high abundance in the coastal area in October 1995. We conclude that the Tsushima Warm Current strongly influenced the South Sea of Korea in 1995 and created strong upwelling front bordering cold upwelled water in the coastal area around Narodo and Sorido Islands. It leads us that these physical structures introduce the favorable environment for the development of C. polykrikoides blooms. We suggest that C. polykrikoides has a bio-physical tolerance of high shear and stress and prefers frontal and upwelling relaxed areas as its habitat. We also find that nutrients were not supplied to the coastal area from the offshore where a low salinity water mass with high nutrients appeared around Jeju Island. Because the strong upwelling front protect the reach of offshore low saline water mass. The main source of nutrients was the upwelled water mass in the coastal area of Wando-Narodo-Sorido.

• 한국어류학회지
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• 제11권1호
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• pp.62-71
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• 1999

동해 남부해역과 대한해협에서 1992년 5월과 11월, 1993년 8월 그리고 1994년 1월에 앨퉁이 난 자치어를 채집하여 계절별 수온전선에 따른 난 자치어의 분포 특성을 분석하였다. 어란은 여름철에, 자치어는 봄철에 출현량이 가장 많았고, 난 자치어의 출현량은 겨울에 가장 적었다. 어란은 4계절 모두 중층이나 저층수의 수온이 $15^{\circ}C$ 이하인 저층냉수가 분포하는 대한해협의 서수도를 포함하여 대만난류와 동해 저층수 사이의 수온 전선역에 주로 출현하였다. 대한해협의 서수도에서 어란의 분포 범위는 계절별 대한해협저층냉수의 구조에 따라 달라진다. 자치어는 어란의 분포 경향과 달리 대륙붕단 주변의 전선역 부근해역에 주로 분포하였으며, 부화 직후의 자어부터 후기자어까지 다양한 크기의 개체가 출현하였다. 앨퉁이는 대륙붕단 주변의 전선역에서 주로 산란하고 부화하며, 대한해협저층냉수의 세력이 강한 여름철에는 많은 량의 어란이 저층냉수와 함께 대한해협으로 유입되는 것으로 판단된다. 대한해협은 앨퉁이 난과 자치어의 남방분포 한계 해역으로 추정된다.

• 한국수산과학회지
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• 제16권4호
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• pp.401-409
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• 1983

1981년과 1982년 $4{\sim}6$월에 한국 남해와 서해 연근해에서 채집된 멸치의 난치어 및 해양관측 자료를 사용하여 수괴배치에 따른 멸치의 난치어의 분포를 분석하였다. 온도전선은 남해에서는 제주도와 대마도를 잇는 선상에서 한국남안연안수와 대마난류간에 형성되었고 서해에서는 태안반도이남해역과 해안선과 평행하게 남북으로 한국서안연안수와 황해냉수간에 형성되었다. 한국남해에서 멸치난은 온도전선 내측인 연안측에서, 멸치 치어는 온도전선을 중심으로 연안측과 외해측으로 분리되어 출현하였다. 그러나 한국서해에서 멸치난과 치어는 온도전선내측과 온도전선역인 $12^{\circ}C$ 이상의 해역에서만 출현하였다. 치어의 체장조성을 보면 남해에서는 연안측에서 전기자어가, 외해측에서 후기자어 및 치어기의 멸치가 주로 출현하였으나, 서해에서는 남부해역에서는 전기자어가 북부해역에서는 후기자어가 주로 출현하였다. 또한 온도전선의 경도가 큰 1981년에는 1982년에 비하여 난과 치어의 분포범위가 크게 제한을 받으므로서 전선의 강약은 난과 치어의 분포에 큰 영향을 주는 것으로 추정된다.

• International Journal of Internet, Broadcasting and Communication
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• 제9권1호
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• pp.18-23
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• 2017

In 2015, 100-car pileup was happened because the safe distance from the car in front did not be kept due to much fog at YoungJong Bridge in South Korea. This is why the road would be benumbed with cold weather in winter. For this weather condition, if the driver of the car in front changed the lane suddenly or suddenly slammed on the brake in fog or freezing area, the braking distance of the real car has to be 2 or 3 times longer than usual. In this paper, we have simulated the function that warns and notice about the fog area or the freezing one in the road using Arduino sensors and Beacon. Also we propose the intelligent traffic system to protect the accidents in winter.

• 환경위생공학
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• 제21권4호
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• pp.61-76
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• 2006

A Line Density algorithm was developed to quantify the sea surface temperature distribution using NOAA Sea Surface Temperature(SST) data and Geographic Information Systems(GIS), In addition, a GIS based automation model was designed to extract the Line Density Indices were determined by applying K-means Cluster. SST data in terms of March to May obtained on the coastal area of the Uljin from 2001 to 2004 in spring were used to make two data sets of average sea water temperature map in terms of year as well as month. From the result it was formed that water temperature gradient in April was the strongest among the other months, In particular very strog formation of oceanic front as well as temperature gradients were observed in front of the coastal area around Wonduk and Jukbyeon countries. Because those coastal area is a confront zone of two cold and a warm. It is expected that the development of a Line Density Algorithm would contribute to quantify of the SST for the research of Sea Surface Front(SSF) related to marine life management and the sea environmental conservation.