6 research outputs found

    Numerical Study on the Observational Error of Sea-Surface Winds at Ieodo Ocean Research Station

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    μˆ˜μΉ˜ν•΄μ„μ„ ν†΅ν•˜μ—¬ 이어도 쒅합해양과학기지 ꡬ쑰물이 λŒ€κΈ° μœ λ™μ— λ―ΈμΉ˜λŠ” 영ν–₯을 λΆ„μ„ν•˜μ˜€κ³ , 이 κ²°κ³Όλ₯Ό λ°”νƒ•μœΌλ‘œ 과학기지에 μ„€μΉ˜λœ ν’μ†μ„Όμ„œμ—μ„œμ˜ μΈ‘μ •κ°’ 였차λ₯Ό ν‰κ°€ν•˜λŠ” 연ꡬλ₯Ό μˆ˜ν–‰ν•˜μ˜€λ‹€. 과학기지 ν˜•μƒμ„ 3μ°¨μ›μœΌλ‘œ λͺ¨λΈλ§ν•˜μ˜€κ³  μˆ˜μΉ˜ν•΄μ„μ„ μœ„ν•œ 격자λ₯Ό μƒμ„±ν•˜μ—¬, Navier-Stokes 방정식 및 λ‚œλ₯˜λͺ¨λΈμ„ μ μš©ν•˜μ—¬ μˆ˜μΉ˜ν•΄μ„μ„ μˆ˜ν–‰ν•˜μ˜€λ‹€. μ„ μ •λœ 자유λ₯˜μ˜ 풍속과 풍ν–₯ 쑰건에 λŒ€ν•˜μ—¬ 과학기지 ꡬ쑰물에 μ˜ν•΄ λ³€ν™”λœ μœ λ™μž₯을 κ³„μ‚°ν•˜κ³ , μ‹€μ œ ν’μ†μ„Όμ„œκ°€ μ„€μΉ˜λœ μœ„μΉ˜μ—μ„œμ˜ 풍속/풍ν–₯ 정보와 자유λ₯˜λ₯Ό λΉ„κ΅ν•˜μ˜€λ‹€. 이λ₯Ό ν†΅ν•˜μ—¬ 자유λ₯˜ λ°©ν–₯ 및 μΈ‘μ • μœ„μΉ˜μ— λ”°λ₯Έ λ°μ΄ν„°μ˜ 정확도와 μ‹ λ’°ν•  수 μžˆλŠ” 데이터 λ²”μœ„λ₯Ό μ•Œμ•„λ³΄μ•˜λ‹€. λ³Έ 연ꡬ 결과둜 κ΄€μΈ‘λœ 해상풍 λ°μ΄ν„°μ˜ ꡬ쑰물 간섭에 μ˜ν•œ 였차 λ²”μœ„λ₯Ό μ •λŸ‰μ μœΌλ‘œ νŒŒμ•…ν•  수 μžˆμ—ˆμœΌλ©°, 과학기지가 μœ„μΉ˜ν•œ μ§€μ μ˜ μ •ν™•ν•œ 해상풍 데이터 μ œκ³΅μ„ μœ„ν•œ 기초 자료둜 ν™œμš©λ  κ²ƒμœΌλ‘œ κΈ°λŒ€λœλ‹€. = The influence of Ieodo Ocean Research Station structure to surrounding atmospheric flow is carefully investigated using CFD techniques. Moreover, the validation works of computational results are performed by the comparison with the observed data of Ieodo Ocean Research station. In this paper, we performed 3-dimensional CAD modelling of the station, generated the grid system for numerical analysis and carried out flow analyses using Navier-Stokes equations coupled with two-equation turbulence model. For suitable free stream conditions of wind speed and direction, the interference of the research station structure on the flow field is predicted. Beside, the computational results are benchmarked by observed data to confirm the accuracy of measured date and reliable data range of each measuring position according to the wind direction. Through the results of this research, now the quantitative evaluation of the error range of interfered gauge data is possible, which is expected to be applied to provide base data of accurate sea surface wind around research stations.λ³Έ μ—°κ΅¬λŠ” ν•œκ΅­ν•΄μ–‘μ—°κ΅¬μ›μ˜ '이어도 μ’…ν•©ν•΄μ–‘κ³Όν•™κΈ°μ§€ν™œμš©μ—°κ΅¬' μ‚¬μ—…μ˜ μ§€μ›μœΌλ‘œ μˆ˜ν–‰λ˜μ—ˆμŒ

    μˆ˜μΉ˜ν•΄μ„μ„ μ΄μš©ν•œ 이어도 기지 ꡬ쑰물이 ν•΄μˆ˜ μœ λ™μ— λ―ΈμΉ˜λŠ” 영ν–₯ 뢄석과 ν•΄λ₯˜ κ΄€μΈ‘ 평가 및 λ³΄μ •λ°©μ•ˆ 연ꡬ = Numerical investigation, calibration method of the interaction between Ieodo ocean research station and ocean current

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    이어도에 κ±΄μ„€λœ λ‹€λͺ©μ  ν•΄μ–‘κ³Όν•™κΈ°μ§€μ—μ„œλŠ” μ£Όμœ„ λŒ€λ₯˜ 및 ν•΄λ₯˜μ˜ 데이터 μˆ˜μ§‘μ„ 톡해 기상, μ–΄μž₯예보 λ“±μ˜ 기초 자료λ₯Ό μ œκ³΅ν•˜λŠ” 것을 ν•œ 가지 λͺ©μ μœΌλ‘œ ν•œλ‹€. 그런데 이어도 기지 ꡬ쑰물에 μ˜ν•œ ν•΄μˆ˜ μœ λ™μ˜ λ³€ν™”λŠ” κ³Όν•™κΈ°μ§€μ˜ κ΄€μΈ‘ 데이터에 영ν–₯을 μ£Όμ–΄ μ •ν™•ν•œ 자료 μˆ˜μ§‘μ„ μ–΄λ ΅κ²Œ ν•˜λ―€λ‘œ, 이어도 기지 ꡬ쑰물이 μ£Όμœ„ μœ λ™μ— λ―ΈμΉ˜λŠ” 영ν–₯을 λΆ„μ„ν•˜κ³  μœ λ™ 정보 관츑을 평가/λ³΄μ •ν•˜λŠ” 방법에 λŒ€ν•œ 연ꡬ가 ν•„μš”ν•˜λ‹€. λ³Έ μ—°κ΅¬μ—μ„œλŠ” 이λ₯Ό μœ„ν•œ κΈ°μ΄ˆμ—°κ΅¬λ‘œ, ν•΄λ₯˜μ™€ ꡬ쑰물 μ‚¬μ΄μ˜ μƒν˜Έ μž‘μš©μ„ λͺ¨μ‚¬ν•  수 μžˆλŠ” μ•Œκ³ λ¦¬μ¦˜μ„ 연ꡬ, μ μš©λ°©λ²•μ„ λ…Όμ˜ν•œλ‹€. κ·Έ κ²°κ³Ό, 3차원 μ „μ‚°μœ μ²΄μ—­ν•™μ„ μ΄μš©ν•œ μˆ˜μΉ˜ν•΄μ„μ„ 톡해 이어도 기지 ꡬ쑰물 및 μˆ˜μ€‘μ•”μ΄ˆκ°€ μ£Όμœ„ μœ λ™μ— λ―ΈμΉ˜λŠ” 영ν–₯을 μ—°κ΅¬ν•˜κ³  μ •ν™•ν•œ 데이터 츑정방법을 μ œμ•ˆν•œλ‹€. = One of the main function of Ieodo Ocean Research Station is to service the information about the weather and fishing grounds condition which are collected through calibrating convection flow and ocean current around the station. However, due to the influence of the station"s structure below sea level, it is difficult to obtain the exact flow data. Therefore, it is required to research on the effect of the structure and the method to evaluate and revise the observed data. In this paper, as a basic study, it deals with the algorithm that simulate the interaction between ocean current and the station structure, followed by discussions about the way to applicate the algorithm. Through 3-dimensional computational fluid dynamics analyses (using Navier-Stokes equations with K-turbulence model), the influence of the station and submerged rocks are quantitatively evaluated, and we would suggest methods how to obtain accurate flow information from the measured rough data

    μˆ˜μΉ˜ν•΄μ„μ„ μ΄μš©ν•œ 이어도 기지 ꡬ쑰물이 ν•΄μˆ˜ μœ λ™μ— λ―ΈμΉ˜λŠ” 영ν–₯ 뢄석과 ν•΄λ₯˜ κ΄€μΈ‘ 평가 및 λ³΄μ •λ°©μ•ˆ 연ꡬ = Numerical Investigation, Calibration Method of the Interaction between Ieodo Ocean Research Station and Ocean Current

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    이어도에 κ±΄μ„€λœ λ‹€λͺ©μ  ν•΄μ–‘κ³Όν•™κΈ°μ§€μ—μ„œλŠ” μ£Όμœ„ λŒ€λ₯˜ 및 ν•΄λ₯˜μ˜ 데이터 μˆ˜μ§‘μ„ 톡해 기상, μ–΄μž₯예보 λ“±μ˜ 기초 자료λ₯Ό μ œκ³΅ν•˜λŠ” 것을 ν•œ 가지 λͺ©μ μœΌλ‘œ ν•œλ‹€. 그런데 이어도 기지 ꡬ쑰물에 μ˜ν•œ ν•΄μˆ˜ μœ λ™μ˜ λ³€ν™”λŠ” κ³Όν•™κΈ°μ§€μ˜ κ΄€μΈ‘ 데이터에 영ν–₯을 μ£Όμ–΄ μ •ν™•ν•œ 자료 μˆ˜μ§‘μ„ μ–΄λ ΅κ²Œ ν•˜λ―€λ‘œ, 이어도 기지 ꡬ쑰물이 μ£Όμœ„ μœ λ™μ— λ―ΈμΉ˜λŠ” 영ν–₯을 λΆ„μ„ν•˜κ³  μœ λ™ 정보 관츑을 평가/λ³΄μ •ν•˜λŠ” 방법에 λŒ€ν•œ 연ꡬ가 ν•„μš”ν•˜λ‹€. λ³Έ μ—°κ΅¬μ—μ„œλŠ” 이λ₯Ό μœ„ν•œ κΈ°μ΄ˆμ—°κ΅¬λ‘œ, ν•΄λ₯˜μ™€ ꡬ쑰물 μ‚¬μ΄μ˜ μƒν˜Έ μž‘μš©μ„ λͺ¨μ‚¬ν•  수 μžˆλŠ” μ•Œκ³ λ¦¬μ¦˜μ„ 연ꡬ, μ μš©λ°©λ²•μ„ λ…Όμ˜ν•œλ‹€. κ·Έ κ²°κ³Ό, 3차원 μ „μ‚°μœ μ²΄μ—­ν•™μ„ μ΄μš©ν•œ μˆ˜μΉ˜ν•΄μ„μ„ 톡해 이어도 기지 ꡬ쑰물 및 μˆ˜μ€‘μ•”μ΄ˆκ°€ μ£Όμœ„ μœ λ™μ— λ―ΈμΉ˜λŠ” 영ν–₯을 μ—°κ΅¬ν•˜κ³  μ •ν™•ν•œ 데이터 츑정방법을 μ œμ•ˆν•œλ‹€. = One of the main function of Ieodo Ocean Research Station is to service the information about the weather and fishing grounds condition which are collected through calibrating convection flow and ocean current around the station. However, due to the influence of the station"s structure below sea level, it is difficult to obtain the exact flow data. Therefore, it is required to research on the effect of the structure and the method to evaluate and revise the observed data. In this paper, as a basic study, it deals with the algorithm that simulate the interaction between ocean current and the station structure, followed by discussions about the way to applicate the algorithm. Through 3-dimensional computational fluid dynamics analyses (using Navier-Stokes equations with K-turbulence model), the influence of the station and submerged rocks are quantitatively evaluated, and we would suggest methods how to obtain accurate flow information from the measured rough data.λ³Έ μ—°κ΅¬λŠ” ν•œκ΅­ν•΄μ–‘μ—°κ΅¬μ›μ˜ 이어도 쒅합해양과학기지ꡬ좕 및 ν™œμš©μ—°κ΅¬(KORDI PM43000)μ‚¬μ—…μ˜ μ§€μ›μœΌλ‘œ μˆ˜ν–‰λ˜μ—ˆμŒ

    Pseudo-compressibility λ°©λ²•μ—μ„œ μ΄μƒμœ λ™ 해석을 μœ„ν•œ Level Set λ°©λ²•μ˜ 적용 = Level Set Method Applied On Pseudo-compressibility Method for the Analysis of Two-phase Flow

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    Level Set 방법을 μ‚¬μš©ν•˜μ—¬ 앑체와 기체의 μ„œλ‘œ λ‹€λ₯Έ 상을 ν•¨κ»˜ ν•΄μ„ν•˜λŠ” 연ꡬλ₯Ό μˆ˜ν–‰ν•˜μ˜€λ‹€. Level Set ν•¨μˆ˜λŠ” μƒμ˜ κ²½κ³„λ©΄μ—μ„œλΆ€ν„° λΆ€ν˜Έλ₯Ό κ°–λŠ” κ±°λ¦¬ν•¨μˆ˜λ‘œ μ •μ˜λ˜λ©°, 계산 κ²©μžμ—μ„œ ν•¨μˆ˜ κ°’μ˜ λΆ€ν˜Έμ— 따라 각 상을 κ΅¬λΆ„ν•˜κ³  λ¬Όμ„±μΉ˜λ₯Ό λΆ€μ—¬ν•œλ‹€. λ³Έ λ…Όλ¬Έμ—μ„œλŠ” λΉ„μ••μΆ•μ„± 유체의 보쑴식에 Level Set ν•¨μˆ˜μ˜ 이동식을 μ—°κ³„ν•˜μ—¬ μ΄μƒμœ λ™μ„ λͺ¨μ‚¬ν•˜λŠ” 지배방정식을 κ΅¬μ„±ν•˜μ˜€μœΌλ©°, 이λ₯Ό pseudo-compressibility λ°©λ²•μœΌλ‘œ ν•¨κ»˜ ν’€μ—ˆλ‹€. 이 λ•Œ λ‹€μ–‘ν•œ λ¬Έμ œμ— 적용이 κ°€λŠ₯ν•˜λ„λ‘ 일반 곑선 μ’Œν‘œκ³„μ—μ„œ 식을 μœ λ„ν•˜μ˜€κ³ , μˆ˜μΉ˜ν•΄μ„μ„ μœ„ν•œ 행렬식듀을 ν•¨κ»˜ μœ λ„ν•˜μ˜€λ‹€. 개발된 해석 μ½”λ“œλ₯Ό ν‘œλ©΄μž₯λ ₯이 μžˆλŠ” 기포 동역학 λ¬Έμ œμ™€ μˆ˜μ€‘μ΅μ— μ˜ν•œ νŒŒλ„ λ°œμƒ λ¬Έμ œμ— μ μš©ν•˜μ—¬ νƒ€λ‹Ήν•œ κ²°κ³Όλ₯Ό 얻을 수 μžˆμ—ˆλ‹€. = In order to analyze incompressible two-phase flow, Level Set method was applied on pseudo-compressibility formulation. Level Set function is defined as a signed distance function from the phase interface, and gives the information of the each phase location and the geometric data to the flow. In this study, Level Set function transport equation was coupled with flow conservation equations, and owing to pseudo-compressibility technique we could solve the resultant vector equation iteratively. Two-phase flow analysis code was developed on general curvilinear coordinate, and numerical tests of bubble dynamics and surging wave problems demonstrate its capability successfully.λ³Έ μ—°κ΅¬λŠ” ν•œκ΅­ν•΄μ–‘μ—°κ΅¬μ›μ˜ '이어도 μ’…ν•©ν•΄μ–‘κ³Όν•™κΈ°μ§€ν™œμš©μ—°κ΅¬(KORDI PE29200)' μ‚¬μ—…μ˜ μ§€μ›μœΌλ‘œ μˆ˜ν–‰λ˜μ—ˆμŒ

    Level Set Method Applied on Pseudo-compressibility Method for the Analysis of Two-phase Flow

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    In order to analyze incompressible two-phase flow, Level Set method was applied on pseudo-compressibility formulation. Level Set function is defined as a signed distance function from the phase interface,and gives the information of the each phase location and the geometric data to the flow. In this study, Level Settechnique we could solve the resultant vector equation iteratively. Two-phase flow analysis code was developedon general curvilinear coordinate, and numerical tests of bubble dynamics and surging wave problems demon-strate its capability successfully.N

    Study on Wind Tunnel Test and 3 Dimensional Numerical Analysis of EARDO Ocean Research Station

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    OAIID:oai:osos.snu.ac.kr:snu2002-01/102/0000004648/43SEQ:43PERF_CD:SNU2002-01EVAL_ITEM_CD:102USER_ID:0000004648ADJUST_YN:NEMP_ID:A001138DEPT_CD:446CITE_RATE:0FILENAME:이어도_쒅합해양과학기지_ν’λ™μ‹€ν—˜_및_3차원_μˆ˜μΉ˜ν•΄μ„μ—_κ΄€ν•œ_연ꡬ.pdfDEPT_NM:기계항곡곡학뢀EMAIL:[email protected]_YN:NCONFIRM:
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