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An Analysis of the Wintertime Diurnal Wind Variation and Turbulent Characteristics over Yongpyong Alpine Slope

용평 알파인 경기장에서 겨울철 바람의 일변화 및 난류 특성분석

  • Jeon, Hye-Rim (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Kim, Byung-Gon (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Eun, Seung-Hee (Department of Atmospheric Environmental Sciences, Gangneung-Wonju National University) ;
  • Lee, Young-Hee (Department of Astronomy and Atmospheric Sciences, Kyungpook National University) ;
  • Choi, Byoung-Cheol (High-impact Weather Research Center, Forecast Research Division, National Institute of Meteorological Studies)
  • 전혜림 (강릉원주대학교 대기환경과학과) ;
  • 김병곤 (강릉원주대학교 대기환경과학과) ;
  • 은승희 (강릉원주대학교 대기환경과학과) ;
  • 이영희 (경북대학교 천문대기과학과) ;
  • 최병철 (국립기상과학원 관측예보연구과 재해기상연구센터)
  • Received : 2016.04.12
  • Accepted : 2016.06.27
  • Published : 2016.09.30

Abstract

A 3D sonic anemometer has been installed at Yongpyong alpine slope since Oct. 23th 2014 to observe the slope winds and to analyze turbulent characteristics with the change in surface cover (grass and snow) and the synoptic wind strength. Eddy covariance method has been applied to calculate the turbulent quantity after coordinate transformation of a planar-fit rotation. We have carefully selected 3 good episodes in the winter season (23 October 2014 to 28 February 2015) for each category (9 days in total), such as grass and snow covers in case of weak synoptic wind condition, and grass cover of strong synoptic wind. The diurnal variations of the slope winds were well developed like the upslope wind in the daytime and downslope wind in the nighttime for both surface covers (grass and snow) in the weak synoptic forcing, when accordingly both heat and momentum fluxes significantly increased in the daytime and decreased in the nighttime. Meanwhile, diurnal variation of heat flux was not present on the snow cover probably in associated with significant fraction of sunlight reflection due to high albedo especially during the daytime in comparison to those on the grass cover. In the strong synoptic regime, the most dominant feature at Yongpyong, only the southeasterly downslope winds were steadily generated irrespective of day and night with significant increases in momentum flux and turbulent kinetic energy as well, which could suggest that local circulations are suppressed by the synoptic scale forcing. In spite of only one season analysis applied to the limited domain, this kind of an observation-based study will provide the basis for understanding of the local wind circulation in the complex mountain domain such as Gangwon in Korea.

Keywords

References

  1. Carrera, M. L., J. R. Gyakum, and C. A. Lin, 2009: Observation study of wind channeling within the St. Lawrence River Valley. J. Appl. Meteor. Climatol., 48, 2341-2361. https://doi.org/10.1175/2009JAMC2061.1
  2. Cuxart, J., and M. A. Jimenez, 2011: Deep radiation fog in a wide closed valley: Study by numerical modeling and remote sensing. Pure. Appl. Geophys., 169, 911- 926, doi:10.1007/s00024-011-0365-4.
  3. Cuxart, J., J. Cunillera, M. A. Jimenez, D. Martinez, F. Molinos, and J. L. Palau, 2011: Study of mesobeta basin flows by remote sensing. Bound.-Layer Meteor., 143, 143-158, doi:10.1007/s10546-0119655-8.
  4. Eun, S. H., S. H. Chae, B. G. Kim, and K. H. Chang, 2011: Effect of urbanization on the light precipitation in the mid-Korean peninsula. Atmosphere, 21, 229-241 (in Korean with English abstract).
  5. Gustavsson, T., M. Karlsson, J. Bogren, and S. Lindqvist, 1998: Development of temperature patterns during clear nights. J. Appl. Meteor., 37, 559-571. https://doi.org/10.1175/1520-0450(1998)037<0559:DOTPDC>2.0.CO;2
  6. Haiden, T., and C. D. Whiteman, 2005: Katabatic flow mechanisms on a low-angle slope. J. Appl. Meteor., 44, 113-126. https://doi.org/10.1175/JAM-2182.1
  7. Han, S.-H., and J.-G. Lee, 2007: A numerical simulation study on the sensitivity of WRF model in the wind field to the steepness of mountain slope. Atmos. Korean Met. Soc., 17, 349-364.
  8. Horst, T. W., and J. C. Doran, 1986: Nocturnal drainage flow on simple slopes. Bound.-Layer Meteor., 34, 263-286. https://doi.org/10.1007/BF00122382
  9. Kim, B.-G., and Coauthors, 2014: An analysis of heavy snowfalls and cold wave and development of its forecast method in Yeongdong. National Institute of Meteorological Science, 35-43.
  10. Lee, X., W. Massman, and B. Law, Eds., 2004: Handbook of micrometeorology: A Guide for surface Flux Measurement and Analysis. Klewer Academic Publishers, 250 pp.
  11. Lindkvist, L., and S. Lindqvist, 1997: Spatial and temporal variability of nocturnal summer frost in elevated complex terrain. Agric. Forest Meteor., 87, 139-153. https://doi.org/10.1016/S0168-1923(97)00021-X
  12. Lindkvist, L., T. Custavsson, and J. Bogren, 2000: A frost assessment method for mountainous areas. Agric. Forest Meteor., 102, 51-67. https://doi.org/10.1016/S0168-1923(99)00087-8
  13. Mahrt, L., 2006: Variation of surface air temperature in complex terrain. J. Appl. Meteor. Climatol., 45, 1481-1493. https://doi.org/10.1175/JAM2419.1
  14. Monti, P., H. J. S. Fernando, M. Princevas, W. C. Chan, T. A. Kowalewski, and E. R. Pardyjak, 2002: Observations of flow and turbulence in the nocturnal boundary layer over a slope. J. Atmos. Sci., 59, 2513-2534. https://doi.org/10.1175/1520-0469(2002)059<2513:OOFATI>2.0.CO;2
  15. Oliver, H. R., 1992: Studies of the energy budget of sloping terrain. Int. J. Climatol., 12, 55-68. https://doi.org/10.1002/joc.3370120106
  16. Papadopoulos, K. H., C. G. Helmis, A. T. Soilemes, J. Kalogiros, P. G. Papageorgas, and D. N. Asimakopoulos, 1997: The structure of katabatic flows down a simple slope. Quart. J. Roy. Meteor. Soc., 123, 1581-1601. https://doi.org/10.1002/qj.49712354207
  17. Sun, J., S. P. Burns, A. C. Delany, S. P. Oncley, T. W. Horst, and D. H. Lenschow, 2003: Heat balance in the nocturnal boundary layer during CASES-99. J. Appl. Meteor., 42, 1649-1666. https://doi.org/10.1175/1520-0450(2003)042<1649:HBITNB>2.0.CO;2
  18. Wilczak, J. M., S. P. Oncley, and S. A. Stage, 2001: Sonic anemometer tilt correction algorithms. Bound.-Layer Meteor., 99, 127-150. https://doi.org/10.1023/A:1018966204465
  19. Whiteman, C. D., 2000: Mountain Meteorology: Fundamentals and applications. Oxford University Press, 376 pp.
  20. Whiteman, C. D., and J. C. Doran, 1993: The relationship between overlying synoptic-scale flows and winds within a valley. J. Appl. Meteor., 32, 1669-1682. https://doi.org/10.1175/1520-0450(1993)032<1669:TRBOSS>2.0.CO;2
  21. Whiteman, C. D., and S. Zhong, 2008: Downslope flows on a lowangle slope and their interactions with valley inversions. I. Observations. J. Appl. Meteor. Climatol., 47, 2023-2038. https://doi.org/10.1175/2007JAMC1669.1
  22. Zoumakis, N. M., G. A. Efstathiou, A. G. Kelessis, J. Triandafyllis, D. Papas, M. Chasapis, M. Petrakakis, and P. Karavelis, 2006: A simple scheme for daytime estimates of surface energy budget in complex terrain. Fresen. Environ. Bull., 15, 923-927.