최소 단어 이상 선택하여야 합니다.
최대 10 단어까지만 선택 가능합니다.
다음과 같은 기능을 한번의 로그인으로 사용 할 수 있습니다.
NTIS 바로가기바다 : 한국해양학회지 = The sea : the journal of the Korean society of oceanography, v.23 no.4, 2018년, pp.153 - 178
변도성 (국립해양조사원 해양과학조사연구실) , 김효원 (국립해양조사원 해양과학조사연구실) , 이주영 (국립해양조사원 해양과학조사연구실) , 이은일 (국립해양조사원 해양과학조사연구실) , 박경애 (서울대학교 지구과학교육과) , 우혜진 (서울대학교 과학교육과)
Most operational uses of wind speed data require measurements at, or estimates generated for, the reference height of 10 m above mean sea level (AMSL). On the Ieodo Ocean Research Station (IORS), wind speed is measured by instruments installed on the lighthouse tower of the roof deck at 42.3 m AMSL....
핵심어 | 질문 | 논문에서 추출한 답변 |
---|---|---|
해상에서 바람의 측정되는 고도가 다양한 이유는 무엇인가? | 일반적으로 해상에서 바람은 선박, 부이, 타워, 외해 플랫폼 등을 이용하여 각기 다른 고도에 풍향‧풍속계를 설치하여 측정하기 때문에 측정되는 고도는 다양하다(Smith 1988; Singh et al., 2013). | |
각기 다른 고도에서 풍향‧풍속계를 이용해 관측한 결과 값은 어디에 활용되어지는가? | , 2013). 이렇게 관측된 평균 풍속은 국제적으로 해상 10 m 기준 고도의 풍속으로 변환시킨 후 기상예측모델의 예측바람 검증, 해양-대기 열수지 계산, 해양순환모델에서 바람응력(wind stress) 입력값 등 여러 방면에 활용된다(Pinson and Hagedorn, 2012; Smith and Dobson, 1984; Oey and Chen, 1992; Sīle et al., 2014). | |
운용용으로 사용되는 풍속자료는 어떻게 측정or생성된 자료인가? | 운용용으로 사용되는 대부분의 풍속자료는 10 m 기준 고도에서 측정 또는 생산된 자료이다. 이 연구는 이어도 해양과학기지 42. |
Andreas, E.L. 1989. Thermal and size evolution of sea spray droplets. Office of Naval Research, CRREL Report pp. 89-11.
Bentamy, A., D. Croize-Fillon and C. Perigaud, 2008. Characterization of ASCAT measurements based on buoy and QuikSCAT wind vector observations. Ocean Sci., 4: 265-274.
Choi, D.-Y., H.-J. Woo, K.-A. Park, D.-S. Byun and E.I. Lee, 2018. Validation of Sea Surface Wind Speeds from Satellite Altimeters and Relation to Sea State Bias - Focus on Wind Measurements at Ieodo, Marado, Oeyeondo Statio. J. Korean Earth Sci. Soc., 39: 139-153.
Chou, K.-H., C.-C. Wu and S.-Z. Lin, 2013. Assessment of the ASCAT wind error characteristics by global dropwindsonde observations. J. Geophys. Res., 118: 9011-9021.
Donelan, M.A., 2018. On the decrease of the oceanic drag coefficient in high winds. J. Geophys. Res., 123: 1485-1501.
Fairall, C.W., E.F. Bradley, D.P. Rogers, J.B. Edson and G.S. Young, 1996. Bulk parameterization of air-sea fluxes for Tropical Ocean-Global Atmosphere Coupled-Ocean Atmosphere Response Experiment. J. Geophys. Res., 101: 3747-3764.
Hus, S.A., E.A. Meindl and D.B. Gilhousen, 1994. Determining the power-law wind-profile exponent under near-neutral stability conditions at sea. Journal of Applied Meteorology, 33: 757-765.
Garratt, J.R., 1977. Review of drag coefficients over oceans and continents. Monthly Weather Review, 105: 915-929.
Kang, K.-M., D.-J. Kim, J.-H. Hwang, C.H. Choi, S.H. Nam, S.J. Kim, Y.-K. Cho, D.-S. Byun and J.Y. Lee, 2017. Establishment of thermal infrared observation system on Ieodo Ocean Research Station for time-series sea surface temperature extraction. J. Korean Soc. Oceanogr., 22: 57-68.
Large, W.G. and S. Pond, 1981. Open ocean momentum flux measurements in moderate to strong winds. Journal of Physical Oceanography, 11: 324-336.
Large, W.G., J. Morzel and G.B. Crawford, 1995. Accounting for surface wave distortion of the marine wind profile in low-level ocean storms wind measurements. Journal of Physical Oceanography, 25: 2959-2971.
Liu, W.T., K.B. Katsaros and J.A. Businger, 1979. Bulk parameterization of air-sea exchange of heat and water vapor including the molecular constraints at the interface. Journal of the Atmospheric Sciences, 36: 1722-1735.
Liu, W.T. and W. Tang, 1996. Equivalent neutral wind. JPL Publication, Pasadena, CA, pp. 96-17.
Moon, I.-J., J.-S. Shim, D.Y. Lee, J.H. Lee, I.-K. Min and K.C. Lim, 2010. Typhoon researches using the Ieodo Ocean Research Station: Part I. Importance and present status of typhoon observation. Atmosphere, Korean Meteorological Society, 20: 247-260.
Oh, H.-M. and K.-J. Ha, 2005. Analysis of marine meteorological characteristics at Ieodo Ocean Research Station from 2003 to 2004. Atmosphere, Korean Meteorological Society, 41: 671-680.
Oh, H., K.-J. Ha and J.-S. Shim, 2014. Analysis for onset of Changma using Ieodo Ocean Research Station Data. Atmosphere, Korean Meteorological Society, 24: 189-196.
Oey, L.Y. and P. Chen, 1992. A model simulation of circulation in the Northeast Atlantic Shelves and Seas. Journal of Geophysical Research, 97: 20087-20115.
Pawlowicz, R., B. Beardsley and S. Lentz, 2002. Classical tidal harmonic analysis including error estimates in MATLAB using T_TIDE. Comput. Geosci, 28: 929-937, doi:10.1016/S0098-3004(02)00013-4.
Peng, S. and Y. Li, 2015. A parabolic model of drag coefficient for storm surge simulation in the South China Sea. Sci. Rep., 5: 15496, doi: 10.1038/srep15496.
Pinson, P. and R. Hagedorn, 2012. Verification of the ECMWF ensemble forecasts of wind speed against analyses and observations. Meteorological Applications, 19: 484-500.
Powell, M.D., P.J. Vickery and T.A. Reinhold, 2013. Reduced drag coefficient for high wind speeds in tropical cyclones. Nature, 422: 279-283.
Powell, M.D., 2008. High Wind Drag Coefficient and Sea Surface Roughness in Shallow Water, Final Report to the Joint Hurricane Testbed. 24 pp.
Sile, T., L. Bekere, D. Cepite-Frisfelde, J. Sennikovs and U. Bethers, 2014. Verification of Numerical Weather Prediction Model Results for Energy Applications in Latvia. Energy Procedia, 59: 213-220.
Singh, P., A. Parekh and R. Attada, 2013. Comparison of a simple logarithmic and equivalent neutral wind approaches for converting buoy-measured wind speed to the standard height: special emphasis to North Indian Ocean, 111: 455-463.
Shim, J.-S., B.-C. Oh and I.-S. Chun, 2003. Influences of Ieodo Ocean Research Station on the ambient wind field. Journal of Korean Society of Coastal and Ocean Engineers, 25: 707-718.
Smith, S.D. 1988. Coefficient for sea surface wind stress, heat flux, and wind profiles as a function of wind speed and temperature. Journal of Geophysical Research, 93: 15468-15472.
Smith, S.D. and F.W. Dobson, 1984. The heat budget at ocean weather station Brave. Atmosphere-Ocean, 22: 1-22.
Spera, D.A. and T.R. Richards, 1979. "Modified power low equations for vertical wind profiles," in Proceedings of the Conference and Workshop on Wind Energy Characteristics and Wind Energy Siting, Portland, Ore, USA, 19-21 June, 1979, pp. 1-10.
Wieringa, J., A.G. Davenport, C.S.B. Grimmond and T.R. Oke, 2001. New revision of Davenport roughness classification. Proceedings of the 3rd European and African Conference on Wind Engineering, Eindhoven, The Netherlands, 2-6 July, 2001, pp. 285-292.
WMO (World Meteorological Organization), 2008. Guidelines for converting between various wind averaging periods in tropical cyclone conditions. Appendix II, pp. 6-10.
Woo, H.-J., K.-A. Park, D.-S. Byun, J.Y. Lee and E.I. Lee, 2018. Characteristics of the Differences between Significant Wave Height at Ieodo Ocean Research Station and Satellite Altimeter-measured Data over a Decade (2004-2016), J. Korean Soc. Oceanogr., 23(1): 1-19.
Zijlema, M., G.P. van Vledder and L.H. holthuijsen, 2012. Bottom friction and wind drag for wave models. Coast. Eng., 65: 19-26.
*원문 PDF 파일 및 링크정보가 존재하지 않을 경우 KISTI DDS 시스템에서 제공하는 원문복사서비스를 사용할 수 있습니다.
출판사/학술단체 등이 한시적으로 특별한 프로모션 또는 일정기간 경과 후 접근을 허용하여, 출판사/학술단체 등의 사이트에서 이용 가능한 논문
※ AI-Helper는 부적절한 답변을 할 수 있습니다.