DOI QR코드

DOI QR Code

The Study of Correlations between Air-Sea Temperature Difference and Precipitation and between Wind and Precipitation in the Yeongdong Coastal Region in Relation to the Siberian High

겨울철 시베리아 고기압과 관련된 영동 해안 강수량과 해기차 및 바람의 상관성에 관한 연구

  • Song, Ji-Ae (National Center for Agro Meteorology) ;
  • Lee, Jae Gyoo (Department of Atmospheric & Environmental Sciences, Gangneung-Wonju National University) ;
  • Kim, Yu-Jin (Department of Atmospheric & Environmental Sciences, Gangneung-Wonju National University)
  • 송지애 (국가농림기상센터) ;
  • 이재규 (강릉원주대학교 대기환경과학과) ;
  • 김유진 (강릉원주대학교 대기환경과학과)
  • Received : 2015.12.11
  • Accepted : 2015.12.31
  • Published : 2016.03.31

Abstract

In this study, the correlations between AST850 and precipitation, and those between WDT and precipitation in the Yeongdong coastal region under the direct/indirect influence of the expansion of cP (continental polar air mass) high were quantitatively analyzed based on the winter season data for the last 20 years, according to surface pressure patterns such as Type 1 (cP high expansion type), Type 2 (cP high expansion + trough type), Type 4 (South trough type), and Type 5 (East Sea trough type). Here, AST850 represents 'sea surface temperature minus temperature on 850 hPa level' and WDT represents 'a speed of 1000 hPa wind projected onto a certain wind direction times precipitation duration in hour'. First, the correlation coefficients between AST850 and precipitation in Type 1, Type 2, and Type 5 cases were 0.253, 0.384, and 0.398 respectively, indicating that a tendency of increasing precipitation linearly with the value of AST850 is slightly presented. In the case of Type 4, however, the coefficient was -0.15, representing almost no linear correlation between AST850 and precipitation. In the correlation between WDT and precipitation, there was the largest correlation coefficient (0.464) between WDT along a direction of $90^{\circ}$ and at EN1 in Type 1 cases. In the case of Type 2, there was the largest correlation coefficient (0.767) between WDT along a direction of $67.5^{\circ}$ and at ES1. In the case of Type 4, there was the largest correlation coefficient (0.559) between WDT along a direction of $22.5^{\circ}$ and at EN2. Finally, in the case of Type 5, there was the largest correlation coefficient (0.945) between WDT along a direction of $315^{\circ}$ and at SE1, representing the largest coefficient among the types. It was found that surface wind directions with the highest correlations to precipitation in the Yeongdong coastal area on winter season were varied according to surface pressure patterns, and that the correlations between WDT and precipitation were higher than those between AST850 and precipitation.

Keywords

References

  1. Anderson, T., and S. Nilson, 1990: Topographically induced convective snowbands over the baltic sea and their precipitation distribution. Amer. Meteor. Soc., 5, 299-312.
  2. Carpenter, D. M., 1993: The lake effect of the great salt lake: Overview and forecast problems. Wea. Forecasting, 8, 181-193. https://doi.org/10.1175/1520-0434(1993)008<0181:TLEOTG>2.0.CO;2
  3. Cho, K.-H., and T.-Y. Kwon, 2012: Orographic and ocean effects associated with a heavy snowfall event over Yeongdong region. Atmosphere, 22, 57-71 (in Korean with English abstract). https://doi.org/10.14191/Atmos.2012.22.1.057
  4. Choi, M.-K., 1994: Heavy snowfall in the Young-dong region accompanied by the southward expansion of cold air toward East Sea. Forecast Technique, 5, 1-10.
  5. Chung, B.-O., 1995: A comparative study on the characteristic of snowfall between Youngdong region and west seaside district at honam region in Korea. M.S. Thesis, Chosun University, 45 pp (in Korean with English abstract).
  6. Chung, K.-B., J.-Y. Kim, and T.-Y. Kwon, 2004: Characteristics of lower-tropospheric wind related with winter precipitation in the Yeongdong region. Atmosphere, 40, 369-380 (in Korean with English abstract).
  7. Hill, F. F., K. A., Browning, and M. J. Bader, 1981: Radar and rain gauge observations of orographic rain over south wales. Quart. J. Roy. Meteor. Soc., 107, 643-670. https://doi.org/10.1002/qj.49710745312
  8. Jhun, J.-G., D.-K. Lee, and H.-A. Lee, 1994: A study on the heavy snowfalls occurred in South Korea. Asia-Pac. J. Atmos. Sci., 30, 97-115 (in Korean with English abstract).
  9. Kim, K.-H., 1993: Correlations between heavy snowfall in the Young-dong region and sea surface temperature. Gang-Won Weather Characteristics, 5, 21-28.
  10. Lee, H., and T.-Y. Lee, 1994: The governing factors ofr heavy snowfalls in Youngdong area. Asia-Pac. J. Atmos. Sci., 30, 179-218 (in Korean with English abstract).
  11. Lee, J. G., 1999: Synoptic structure causing the difference in observed snowfall amount at taegwallyong and Kangnung: Case study. Asia-Pac. J. Atmos. Sci., 35, 319-334 (in Korean with English abstract).
  12. Lee, J. G., and Y. J. Kim, 2008: A numerical case study examining the orographic effect of the taebaek mountains on snowfall distribution over the Yeongdong area. Atmosphere, 18, 364-386 (in Korean with English abstract).
  13. Lee, J. G., and Y. J. Kim, 2009: A numerical case study examining the orographic effect of the northern mountains complex on snowfall distribution over the Yeongdong area. Atmosphere, 19, 345-370 (in Korean with English abstract).
  14. Lee, J.-H., S.-H. Eun, B.-G. Kim, and S.-O. Han, 2012: An analysis of low-level stability in the heavy snowfall event observed in the Yeongdong region. Atmosphere, 22, 209-219 (in Korean with English abstract). https://doi.org/10.14191/Atmos.2012.22.2.209
  15. Lee, T.-Y., and Y.-Y. Park, 1996: Formation of a mesoscale trough over the Korean peninsula during an excursion of Siberian high. J. Meteor. Soc. Japan, 74, 299-323. https://doi.org/10.2151/jmsj1965.74.3_299
  16. Nam, H.-G., B.-G. Kim, S.-O. Han, C. K. Lee, and S.-S. Lee, 2014: Characteristics of easterly-induced snowfall in Yeongdong and its relationship to air-sea temperature difference. Asia-Pac. J. Atmos. Sci., 50, 541-552. https://doi.org/10.1007/s13143-014-0044-3
  17. Neiman, P. J., F. M. Ralph, A. B. White, D. E. Kingsmill, and P. O. G. Persson, 2002: The statistical relationship between upslope flow and rainfall in california's coastal mountains: Observations during CALJET. Mon. Wea. Rev., 130, 1468-1492. https://doi.org/10.1175/1520-0493(2002)130<1468:TSRBUF>2.0.CO;2
  18. Song, I.-S., 1992: Understanding Statistics - including SPSS analysis methods. Hakjisa, 720 pp (in Korean).
  19. Song, J.-A., 2015: The Study of Synoptic Patterns in Favor of Heavy Snowfall in the Yeongdong Area and Predictors for Heavy Snowfall Amounts. M.S. Thesis, Gangneung-Wonju National University, 91 pp (in Korean with English abstract).
  20. Yoo, C.-S., and B.-O. Chung, 1996: A comparative study on the characteristic of snowfall between Youngdong region and west seaside district at honam region in Korea. Natural Sci. Res., 19, 131-158 (in Korean with English abstract).
  21. Waldstreicher, J. S., 2002: A foot of snow from a 3000-foot cloud: The ocean-effect snowstorm of 14 January 1999. Bull. Amer. Meteor. Soc., 83, 19-22. https://doi.org/10.1175/1520-0477(2002)083<0019:AFOSFA>2.3.CO;2

Cited by

  1. Interannual variability of winter precipitation linked to upper ocean heat content off the east coast of Korea pp.08998418, 2017, https://doi.org/10.1002/joc.5354
  2. Characteristics of Meteorological Elements Change Associated with Heavy Snowfall in the Youngdong Area, Gangwon Province in the Past Five Years vol.10, pp.3, 2019, https://doi.org/10.15531/KSCCR.2019.10.3.227