• Ocean Science Journal
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• 제43권2호
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• pp.115-126
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• 2008

Direct measurements of four radiative components at air-sea boundary layer were conducted in the southern Yellow Sea during three cruises (seasons) in 2007. Simultaneous observations of meteorological (cloud cover, air temperature and humidity) and oceanographic (sea surface temperature) parameters were carried out. Observational results of radiative fluxes and meteorological and oceanographic parameters are presented. Mean diurnal cycles of four radiative components, net radiation, and sea surface albedo are calculated to achieve averages in different seasons. Net radiative fluxes in three seasons (winter, spring, autumn) are 8, 146, $60\;W/m^2$, respectively. Comparisons between the observed radiative fluxes and those estimated with formulas are taken.

• 한국해양학회지
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• 제18권2호
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• pp.104-110
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• 1983

海洋 亂流境界層內 亂流運動量輸送의 斷續性 現象에 對하여 그 本質을 把握 하고 流體力學的 인 의미를 규명하기 위한 영구를 기원했다.또한 단속성 현상과 작비현상의 상호관계도 아울러 연구했다. 본 연구를 통해 난류경계층내에서도 중간층에 속하는 z/h=0.067층에서는 단속성의 크기가 평균난류운동량 수송의 408배의 달하고 상부층 즉 z/h=0.1층에서는 270배에 달함이 밝혀져,이제까지 보고되었던 Gordon(1974)이나 Heathersaw(1974)의 30배의 월등히 크다는 것이 새로운 사실이다. 일부 학자들은 단속성현상을 자기현상의 반영 또는 자기의 유통계의 부딪혀 나타나는 현상이라고 해석한바 있으나 (Gordon,1974; Heathersaw,1974),본 연구에서 밝혀진바에 의하면,이는 마찰 Reynolds 수가>$10^{5}$인 실제해양의 난류경계층내 난류운동의 특징이라는 사실이다.

• 한국유체기계학회 논문집
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• 제13권2호
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• pp.12-17
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• 2010

A kind of disk-shape boundary layer pump is designed numerically by using a software of computational fluid dynamics, which is widely used for the special purposes such as artificial hearts, bio-fluidics and transportation of oceanic lives, etc. From the numerical simulation with an axisymmetric model, some benchmark problems are tested and compared with experimental results. The performance of disk pump is graphically visualized from the computational results, and converted to the dimensionless parameters. Finally, the obtained numerical data in the present investigation can be used for the baseline for new design to achieve a more efficient disk pump.

• 한국해양학회지
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• 제16권1호
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• pp.12-23
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• 1981

A numerical experiment is made in order to clarify the mechanism of the upwelling phenomenon along the coast near the poleward edge of the western boundary current. The possibility of the upwelling is suggested from the analysis of the observational data in the east of Honshu, Japan, and in the south eastern coast of Korean Peninsula. This upwelling phenomenon is very deep and can be traced to the bottom layer. The upwelling phenomenon seems to be a general oceanic feature which characterizes the region along the west coast near the poleward edge of the western boundary current. This experiment is simulating the oceanic condition of the transition region between Kuroshio front and the Oyashio front in the east of Honshu, Japan. The possible explanations of the causes of the upwelling are as follows;In the interior of the modeled ocean the cold heavy water supplied from the north and the warm light water from the south make the north-south gradient of the pressure field and accelerate the eastward current to produce the h-orizontal divergence feld near the west coast. The divergence is compensated by the upwelling near the separation region. Another one is that the upwell-ed cold water strengthen constantly the pressure gradient which is balanced by the northward current and is weakened by the horizontal diffusion.

• 한국환경과학회지
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• 제3권2호
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• pp.129-140
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• 1994

An intermediate atmosphere-ocean coupled model appropnate for the study of El Nino has been developed. The model is not only economic to use but also contains several most important physical processes. The geometrical effects which were not confided in the previous intermediate model study of Ahn (1990), are included in the model for more realistic simulation of the event. The results show that the individual models respond appropriately to the given boundary conditions. At the same time, in the coupled model experiment, ENSO-like oceanic and atmospheric anomalies are also well simulated under an external triggering similar to the initiation forcing of ENSO. It is expected that this type of model can be effectively used for the. study and simulation of El Nido. More improvement of modeling may be Possible after inclusion of subsequent processes such as inclusion of ocean mixed layer dynamics.

• Journal of the korean society of oceanography
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• 제34권4호
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• pp.231-235
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• 1999

A simple analytic model for estimating the volume transport of the Tsushima Current is considered by assuming that the transports through the connecting channels, the Korea and Tsugaru Straits, are geostrophically controled. The model gives a much simpler form of solution than that by Minato and Kimura (1980). It depends no longer on the geometry of the marginal sea and on the thickness of western boundary layer relative to the dimension of the ocean, but considers the geometry of the connecting channels ignored by Nof (1993). The external parameters turn out to be the oceanic meridional sea level difference between the two channels, the depth of the channels and the meridional position of the marginal sea. For typical value of the depth ratio of the channels to the ocean, the model gives an estimate of the Tsushima Current transport of acceptable magnitude.

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 2002년도 추계학술대회 논문집
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• pp.343-343
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• 2002

This study examines the influence of long-range transport of dust particles and air pollutants on both local/regional DMS oxidation chemistry and the distribution of sulfur compounds at Jeju Island (33.17$^{\circ}$ N. 126.10$^{\circ}$ E) during the Asian dust-storm(ADS) period in April 2001. The atmospheric concentrations of these sulfur species were measured at a ground station on Jeju Island. Korea as Part of the ACE-Asia intensive operation. Three ADS events were observed during the periods of 10-12, 13-14. and 25-26 April. respectively. The concentrations of DMS and CS$_2$ were higher during the ADS period than during the non-Asian-dust-storm (NADS) period. Conversely. a difference in SO$_2$ levels during the ADS period was not distinguishable from those during the NADS period. The diurnal variation pattern of DMS observed was largely different from that in the remote marine boundary layer. DMS loss by NO$_3$ in the atmospheric boundary layer was dominant due to significantly high NOx levels influenced by the long-range transport of pollutants from East Asia to Jeju Island The DMS maximum during the ADS period was observed in the late afternoon. The oceanic fluxes of DMS during the ADS and NADS periods were estimated to be 5.7$\pm$2.3 and 2.9 (+2.8/-1.5) mole m$^{-2}$ day$^{-1}$ . respectively. The contribution of oxidized DMS to SO$_2$ levels at Jeju Island during the study period was found to be insignificant.

• 한국해양학회지:바다
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• 제20권2호
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• pp.102-118
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• 2015

본 연구에서는 국제 공동 해양 재분석 자료 비교 프로젝트 결과를 요약하였다. 다양한 재분석 자료 생산 시스템의 종류 및 특성을 소개하였으며, 대표적인 8가지 해양 변수(열용량, 열염분 높이, 해수면 높이, 표층 열속, 혼합층 깊이, 아표층염분, $20^{\circ}C$ 등온선 깊이, 해빙)에 대한 전지구 해양 자료 동화 모델 성능을 비교 분석하였다. 일반적으로 단일 재분석 자료 결과보다 앙상블 평균 값이 비교적 높은 성능을 나타내었으나, 검증 변수와 해역에 따라 서로 다른 특징을 보였다. 해양 변수 중에는 염분 및 해빙 변동이 모델간 가장 큰 편차를 보였다. 심층 해역, 남극해, 서안 경계 해역을 포함한 연안역에서는 공통적으로 객관 분석장과 동화 모델간의 편차가 크게 나타났다. 국내에서도 독립적으로 운영되고 있는 해양 자료 동화 모델간의 비교 분석 프로그램이 추진되어, 향후 관련된 국제 공동 연구에 활발히 참여할 수 있는 기회가 확대되기를 기대한다.

• 한국해양학회지:바다
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• 제29권3호
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• pp.139-152
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• 2024

이 연구에서는 GFDL (Geophysical Fluid Dynamics Laboratory)에서 개발한 해양순환모델인 MOM6 (Modular Ocean Model Version 6)를 사용하여 저해상도 전지구 해양순환모델의 성능을 평가하고 개선 방안을 모색하기 위해 다양한 민감도 실험을 수행하였다. 특히, ePBL (energetics based planetary boundary layer) 혼합층 방안의 적용, 조석 처방, 그리고 하이브리드 수직격자체계의 도입이 모델의 표층 수온과 염분 모의 성능에 미치는 영향을 분석하였다. 연구 결과, ePBL 혼합층 방안은 적도 태평양에서의 혼합층 두께의 과대 모의와 고온 편향을 완화하는 데 효과적이었으며, 조석 처방은 황해와 동해에서 해양 구조를 개선하는데 일부 기여하였다. 또한, 하이브리드 수직격자체계는 수온 및 염분의 수직 구조를 보다 정확하게 모의할 수 있게 하여 모델의 성능을 개선하였다. 이 연구는 해양순환모델의 정확성을 높이기 위한 구체적인 방안을 제시하고 있으며, 전지구적인 해양 및 기후 모델링의 성능 개선에 기여할 수 있을 것으로 기대한다.

• Ocean and Polar Research
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• 제30권3호
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• pp.313-324
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• 2008

In order to understand the variation of ENSO-related oceanic environments in the tropical and North Pacific Ocean, spatio-temporal variations of sea surface temperature anomaly (SSTA) and sea surface height anomaly (SSHA) are analyzed from distributions of complex empirical orthogonal functions (CEOF). Correlations among warm pool variation, southern oscillation index, and ocean surface currents were also examined with respect to interannual variability of the warm pool in western tropical Pacific. Spatio-temporal distributions of the first CEOF modes for SSTA and SSHA indicate that their variabilities are associated with ENSO events, which have a variance over 30% in the North Pacific. The primary reasons for their variabilities are different; SST is predominantly influenced by the change of barrier layer thickness, while SSH fluctuates with the same phase as propagation of an ENSO episode in the zonal direction. Horizontal boundary of warm pool area, which normally centered around $149^{\circ}E$ in the tropics, seemed to be expanded to the middle and eastern tropical regions by strong zonal currents through the mature phase of an ENSO episode.