DOI QR코드

DOI QR Code

Observation and Analysis of Turbulent Fluxes Observed at Ieodo Ocean Research Station in Autumn 2014

2014년 가을철 이어도 종합과학기지에서의 난류 플럭스의 관측 및 분석

  • Yun, Junghee (Department of Atmospheric Sciences, Pusan National University) ;
  • Oh, Hyoeun (Department of Atmospheric Sciences, Pusan National University) ;
  • Ha, Kyung-Ja (Department of Atmospheric Sciences, Pusan National University)
  • 윤정희 (부산대학교 지구환경시스템학부) ;
  • 오효은 (부산대학교 지구환경시스템학부) ;
  • 하경자 (부산대학교 지구환경시스템학부)
  • Received : 2015.09.10
  • Accepted : 2015.11.28
  • Published : 2015.12.31

Abstract

This study investigates the characteristics of turbulent fluxes observed at Ieodo Ocean Research Station (IORS) in autumn 2014. The 10 Hz IORS data is quality controlled and calculated to be the 30 minutes turbulent fluxes. The quality control consists of five steps: a weather check, Vickers and Mahrt (VM) sequential check, VM parallel check, flag check, and direction check. Since the IORS is an open-sea station with no orographic influence, there are no significant diurnal variations for the turbulent fluxes and 10 m wind speed. According to stabilities, the unstable and semi-unstable states appear more than 28% and 70% in autumn, respectively and they have strong winds of over $10m\;s^{-1}$. In addition, the turbulent fluxes increase with increasing wind speed. In particular, the latent heat flux and its deviations are clearly shown because the latent heat flux is influenced by the change of both the sea surface roughness and wave height induced by the wind. To demonstrate the changes of the turbulent fluxes before and after typhoon, Vongpong (1419), which is the most intense typhoon affecting the Korean Peninsula in 2014, is considered. The turbulent flux fluctuates in accordance with the location of Vongpong. The turbulent fluxes have a large (small) variation when Vongpong approaches (retreats) at the IORS. The overall results represent that the IORS data helps us understand physical processes related to air-sea interaction by providing the valuable and reliable observed data.

Keywords

References

  1. Andreas, E. L., and J. Decosmo, 2002: The signature of sea spray in the hexos turbulent heat flux data. Bound.-Layer Meteor., 103, 303-333. https://doi.org/10.1023/A:1014564513650
  2. Charnock, H., 1955: Wind stress on a water surface. Quart. J. Roy. Meteor. Soc., 81, 639-640.
  3. De Szoeke, S. P., J. B. Edson, J. R. Marion, C. W. Fairall, and L. Bariteau, 2015: The MJO and Air-Sea Interaction in TOGA COARE and DYNAMO. J. Climate, 28, 597-622. https://doi.org/10.1175/JCLI-D-14-00477.1
  4. Frankignoul, C., A. Czaja, and B. L'Heveder, 1998: Air-sea feedback in the North Atlantic and surface boundary conditions for ocean models. J. Climate, 11, 2310-2324. https://doi.org/10.1175/1520-0442(1998)011<2310:ASFITN>2.0.CO;2
  5. Hsiung, J., 1985: Estimates of global oceanic meridional heat transport. J. Phys. Oceanogr., 15, 1405-1413. https://doi.org/10.1175/1520-0485(1985)015<1405:EOGOMH>2.0.CO;2
  6. Jang, H.-Y., and S.-Y. Yeh, 2013: Analysis of Atmosphere-Ocean Interactions over South China Sea and its Relationship with Northeast Asian Precipitation Variability during Summer. Atmosphere, 23, 283-291. https://doi.org/10.14191/Atmos.2013.23.3.283
  7. Kitoh, A., and O. Arakawa, 1999: On overestimation of tropical precipitation by an atmospheric GCM with prescribed SST. Geophys. Rese. Lett., 26, 2965-2968. https://doi.org/10.1029/1999GL900616
  8. Kunoki, S., A. Manda, Y.-M. Kodama, S. Iizuka, K. Sato, I. Fathrio, T. Mitsui, H. Seko, Q. Moteki, S. Minobe, and Y. Tachibana, 2015: Oceanic influence on the Baiu frontal zone in the East China Sea. J. Geophys. Res., 120, 449-463.
  9. Li, Z., S. Zhaobo, N. Donghong, and Z. Gang, 2004: Impact of previous Winter kuroshio SSTA on Summer rainfall in China. Acta Oceano Sinica, 19, 76-82.
  10. Liu, W. T., K. B. Katsaros, and J. A. Businger, 1979: Bulk parameterization of air-sea exchanges of heat and water vapor including the molecular constraints at the interface. J. Atmos. Sci., 36, 1722-1735. https://doi.org/10.1175/1520-0469(1979)036<1722:BPOASE>2.0.CO;2
  11. 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 Reserch Station: Part I. Importance and Present Status of Typhoon Observation, Atmosphere, 20, 247-260.
  12. Oh, H.-M., and K.-J. Ha, 2005: Analysis of marine meteorological characteristics at Ieodo Ocean Research Station from 2003 to 2004. Atmosphere, 41, 671-680.
  13. Oh, H.-M., K.-J. Ha, J.-S. Shim, Y.-K. Hyun, and K.-S. Yun, 2007: Seasonal characteristics of turbulent fluxes observed at Ieodo Ocean Research Station. Atmosphere, 17, 421-433.
  14. Oh, H.-M., K.-J. Ha,, K.-Y. Heo, K.-E. Kim, S.-J. Park, J.-S. Shim, and L. Mahrt, 2010: On drag coefficient parameterization with post processed direct fluxes measurements over the ocean. Asia-Pac. J. Atmos. Sci., 46, 513-523. https://doi.org/10.1007/s13143-010-0030-3
  15. Oh, H.-M., K.-E. Kim, K.-J. Ha, L. Mahrt, and J.-S. Shim, 2011: Quality control and tilt correction effects on the turbulent fluxes observed at an ocean platform. J. Appl. Meteor. Climatol., 50, 700-712. https://doi.org/10.1175/2010JAMC2367.1
  16. Oh, H., K.-J. Ha, and J.-S. Shim, 2014: Analysis for Onset of Changma Using Ieodo Ocean Research Station Data. Atmosphere, 24, 189-196. https://doi.org/10.14191/Atmos.2014.24.2.189
  17. Oost, W. A., C. M. J. Jacobs, and C. Van Oort, 2000: Stability effects on heat and moisture fluxes at sea. Bound.-Layer Meteor., 95, 271-302. https://doi.org/10.1023/A:1002678429212
  18. Potter, H., H. C. Graber, N. J. Williams, C. O. Collins III, R. J. Ramos, and W. M. Drennan, 2015: In situ measurements of momentum fluxes in typhoons. J. Atmos. Sci., 72, 104-118. https://doi.org/10.1175/JAS-D-14-0025.1
  19. Roxy, M., Y. Tanimoto, B. Preethi, P. Terray, and R. Krishnan, 2013: Intraseasonal SST-precipitation relationship and its spatial variability over the tropical summer monsoon region. Clim. Dynam., 41, 45-61. https://doi.org/10.1007/s00382-012-1547-1
  20. Stull, R. B., 1988: An introduction to boundary layer meteorology. Kluwer academic publishers, 670 pp.
  21. Subrahamanyam, D. B. and R. Ramachandran, 2002: Airsea interface fluxes over the Indian Ocean during INDOEX, IFP-99. J. of Atmos. and Solar-Terr. Phys., 64, 291-305. https://doi.org/10.1016/S1364-6826(01)00091-8
  22. Tokinaga, H., Y. Tanimoto, S.-P. Xie, T. Sampe, H. Tomita, and H. Ichikawa, 2009: Ocean frontal effects on the vertical development of clouds over the western North Pacific: In situ and satellite observations. J. Climate, 22, 4241-4260. https://doi.org/10.1175/2009JCLI2763.1
  23. Vickers, D., and L. Mahrt, 1997: Quality control and flux sampling problems for tower and aircraft data. J. Atmos. Oceanic. Technol., 14, 512-526. https://doi.org/10.1175/1520-0426(1997)014<0512:QCAFSP>2.0.CO;2
  24. Wallace, J. M., and P. V. Hobbs, 2006: Atmospheric Science: An Introductory Survey. Academic Press, 483 pp.
  25. Wu, R., B. P. Kirtman, and K. Pegion, 2006: Local air-sea relationship in observations and model simulations. J. Climate, 19, 4914-4932. https://doi.org/10.1175/JCLI3904.1
  26. Xu, H., M. Xu, S.-P. Xie, and Y. Wang, 2011: Deep Atmospheric Response to the Spring Kuroshio over the East China Sea. J. Climate, 24, 4959-4972. https://doi.org/10.1175/JCLI-D-10-05034.1
  27. Zhang, L., C. Guan, C. Sun, S. Gao, and S. Yu, 2015: Upper Ocean Thermal Responses to Sea Spray Mediated Turbulent Fluxes during Typhoon Passage. Adv. Meteorol., 2015. [Available online at http://dx.doi.org/10.1155/2015/752947.].
  28. Zhang, Y., and W. Perrie, 2001: Feedback mechanisms for the atmosphere and ocean surface. Boundary-Layer Meteorol., 100, 321-348. https://doi.org/10.1023/A:1018996505248