DOI QR코드

DOI QR Code

Characteristics of Rainfall Systems Accompanied with Changma Front at Chujado in Korea

You, C.H.;Lee, D.I.;Jang, S.M.;Jang, M.;Uyeda, H.;Shinoda, T.;Kobayashi, F.

  • Published : 20100000

Abstract

The rainy season from June to July in the East Asia is called the Changma in Korea, the Meiyu in China, or the Baiu in Japan. The mesoscale convective systems which occur near a front frequently lead to severe weather phenomenon such as localized gust and heavy rainfall. An intensive field experiment was conducted at Chujado (33.95°N, 126.28°E) to find out the characteristics of the precipitating system using information such as the raindrop size distribution, kinematic features during a Changma period between June 21 2007 and July 11 2007. Different characteristics of three identified rainfall cases in a Changma frontal precipitation system occurred from 5 to 6 July in 2007 at Chujado area have been identified. Based on the radar reflectivity and raingage at Chujado, each rainfall system maintained for 7 hours, 4 hours, and 9 hours, respectively. According to the analysis of a total vertical wind shear (TVWS) and a directional vertical wind shear (DVWS), the temperature gradient was the strongest near the surface and both warm and cold advections were occurred in all cases but at different levels. The deep warm advection was related to the longer rainfall lifetime and stronger rainrate, but smaller raindrop size. The unstable atmospheric condition, which has cold advection at the surface and warm advection in higher level, caused the larger size diameter of raindrop. The echo top height of 30 dBZ was around 6 km in the two rainfall systems and around 4 km in the other one. The number concentrations of raindrop has turning point at the drop size of 2 mm in diameter. The stronger (weaker) updraft and downdraft were also related to the decreased number concentration of smaller (larger) size drops and increased that of the larger (smaller) drops.

Keywords

References

  1. Akiyama, T., 1973: The large-scale aspects of the characteristics features of the Baiu front. Pap. Meteorol. Geophys., 24, 157-188
  2. Armijo, L., 1969: A theory for the determination of wind and precipitation velocities with Doppler radars. J. Atmos. Sci., 26, 570-575 https://doi.org/10.1175/1520-0469(1969)026<0570:ATFTDO>2.0.CO;2
  3. Biggerstaff, M. I., and R. A., Houze Jr., 1991: Kinematic and precipitation structure of the 10-11 June, 1985 squall line. Mon. Wea. Rev., 119, 3034-3065 https://doi.org/10.1175/1520-0493(1991)119<3034:KAPSOT>2.0.CO;2
  4. Choi, Y. J., and J. C., Nam, 2006: Introduction of phase I KEOP. Proc. Spring Meeting of Korean Meteor. Soc., Gwangju, Korea, KMS, 384-385. (in Korean)
  5. Ding, Y. H., and J. C. L. Chan, 2005: The East Asian summer monsoon:an overview, Meteor. Atmos. Phys., 89, 117-142 https://doi.org/10.1007/s00703-005-0125-z
  6. Ding, Y. H., C. Y. Li, and Y. J. Liu, 2004: Overview of the South China Sea monsoon experiment. Adv. Atmos. Sci., 21, 343-360 https://doi.org/10.1007/BF02915563
  7. Holton, J. R., 1979: An Introduction to Dynamic Meteorology. Academic Press, 391 pp
  8. Ishihara, M., A. Tabata, K. Akaeda, T. Yokoyama, and H. Sakakibara, 1992: The structure of a subtropical squall line observed with a Doppler radar. Tenki, 39, 727-743. (in Japanese)
  9. Ishihara, M., Y. Fujiyoshi, A. Tabata, H. Sakakibara, K. Akaeda, and H. Okamura, 1995: Dual Doppler radar analysis of an intense mesoscale rainband generated along the Baiu front in 1988: Its kinematical structure and maintenance process. J. Meteor. Soc. Japan, 73, 139-163
  10. Kim, S. S., C. H. Chung, S. U. Park, and B. S. Lee, 1983: The characteristic structural differences of the rainy front (Changma front) between the wet and dry seasons. J. Korean Meteor. Soc., 19, 12-32. (in Korean with English abstract)
  11. Kozu, T., and K. Nakamura, 1991: Rainfall parameter estimation from dual-radar measurements combining reflectivity profile and pathintegrated attenuation. J. Atmos. Oceanic Technol., 8, 259-271 https://doi.org/10.1175/1520-0426(1991)008<0259:RPEFDR>2.0.CO;2
  12. Lau, K. M., Y. H. Ding, J. T. Wang, R. Johnson, R. Cifelli, J. Gerlach, O. Thjiely, T. Rikebbach, S. C. Tsay, and P. H. Lin, 2000: A report of the field operation and early results of the South China Sea monsoon experiment (SCSMEX). Bull. Amer. Meteor. Soc., 81, 1261-1270 https://doi.org/10.1175/1520-0477(2000)081<1261:AROTFO>2.3.CO;2
  13. Lee, D. K., H. R. Kim, and S. Y. Hong, 1998: Heavy rainfall over Korea during 1980-1990. Korean J. Atmos. Sci., 1, 32-50
  14. Lin, Y. J., R. W. Pasken, and H. W. Chang, 1991: The structure of a subtropical prefrontal convective rainband. Part I: Mesoscale kinematic structure determined from dual Doppler measurements. Mon. Wea. Rev., 120, 1816-1836
  15. Matsumoto, S., S. Yoshizumi, and M. Takeuchi, 1970: On the structure of the "aiu Front"and the associated intermediate scale disturbances in the lower atmosphere. J. Meteor. Soc. Japan, 48, 479-491 https://doi.org/10.2151/jmsj1965.48.6_479
  16. Matsumoto, S., S. Yoshizumi, and M. Takeuchi, 1971: Characteristic feature of Baiu front associated with heavy rainfall. J. Meteor. Soc. Japan, 49, 267-281
  17. Miller, L. J., and S. M. Fredric, 1998: Custom Editing and Display of Reduced Information in Cartesian space (CEDRIC) manual. National Center for Atmospheric Research, 130 pp
  18. Moteki, Q., H. Uyeda, T. Maesaka, T. Shinoda, M. Yoshizaki, and T. Kato, 2004: Structure and development of two merged rainbands observed over the East China Sea during X-BAIU-99 PART I: Meso- $\beta$-scale structure and development processes. J. Meteor. Soc. Japan, 82, 19-24 https://doi.org/10.2151/jmsj.82.19
  19. NCAR, 1999: Sorted Position Radar Interpolation (SPRINT) manual. National Center for Atmospheric Research, 76 pp
  20. Ninomiya, K., 1978: Heavy rainfalls associated with frontal depression in Asia subtropical humid region. PART I: Synoptic-scale features. J. Meteor. Soc. Japan, 56, 253-266
  21. Ninomiya, K., and T. Akiyama, 1992: Multi-scale features of Baiu, the Summer Monsoon over Japan and East Asia. J. Meteor. Soc. Japan, 70, 467-495
  22. O’Brien, J. J., 1970: Alternative solution to the classical vertical velocity problem. J. Appl. Meteorol., 9, 197-203 https://doi.org/10.1175/1520-0450(1970)009<0197:ASTTCV>2.0.CO;2
  23. Oh, J. H., W. T. Kwon, and S. B. Ryoo, 1997: Review of the researches on Changma and future observational study (KORMEX). Adv. Atmos. Sci., 14, 207-222 https://doi.org/10.1007/s00376-997-0020-2
  24. Ray, P. S., K. K. Wagner, K. W. Johnson, J. J. Stephens, W. C. Bumgarner, and E. A. Mueller, 1978: Triple-Doppler observations of a convective storm. J. Appl. Meteorol., 17, 1201-1212 https://doi.org/10.1175/1520-0450(1978)017<1201:TDOOAC>2.0.CO;2
  25. Ray, P. S., C. L. Ziegler, W. Bumgarner, and R. J. Serafin, 1980: Singleand multiple-Doppler radar observations of tornadic storms. Mon. Wea. Rev., 108, 1607-1625 https://doi.org/10.1175/1520-0493(1980)108<1607:SAMDRO>2.0.CO;2
  26. Ray, P. S., A. Robinson, and Y. Lin, 1991: Radar analysis of a TAMEX frontal system. Mon. Wea. Rev., 119, 2519-2539 https://doi.org/10.1175/1520-0493(1991)119<2519:RAOATF>2.0.CO;2
  27. Takahashi, N., H. Uyeda, K. Kikuchi, and K. Iwanami, 1996: Mesoscale and convective scale features of heavy rainfall events in lat period of the Baiu season in July 1988, Nagasaki Prefecture. J. Meteor. Soc. Japan, 74, 539-561
  28. Teng, J. H., C. S. Chen, T. C. C. Wang, and Y. L. Chen, 2000: Orographic effects on a squall line system over Taiwan. Mon. Wea. Rev., 128, 1123-1138 https://doi.org/10.1175/1520-0493(2000)128<1123:OEOASL>2.0.CO;2
  29. Ulbrich, C. W., 1983: Natural variations in the analytical form of the raindrop size distribution. J. Climate Appl. Meteor., 22, 1764-1775 https://doi.org/10.1175/1520-0450(1983)022<1764:NVITAF>2.0.CO;2
  30. Yoshizaki, M., T. Kato, Y. Tanaka, H. Takayama, Y. Shoji, H. Seko, K. Arao, K. Manabe, and Members of X-BAIU-98 Observation, 2000: Analytical and numerical study of the 26 June 1998 orographic rainband observed in Western Kyushu, Japan. J. Meteor. Soc. Japan, 78, 835-856

Cited by

  1. Environment and morphology of mesoscale convective systems associated with the Changma front during 9-10 July 2007 vol.30, pp.8, 2012, https://doi.org/10.5194/angeo-30-1235-2012
  2. An Analysis of Precipitation Systems Developed near Jeju Island in Korea during the Summer Monsoon, 2006 vol.33, pp.5, 2012, https://doi.org/10.5467/jkess.2012.33.5.377
  3. A Comparative Study of Cloud-Precipitation Microphysical Properties between East Asia and Other Regions vol.91, pp.4, 2010, https://doi.org/10.2151/jmsj.2013-406
  4. Decadal Variation in Raindrop Size Distributions in Busan, Korea vol.2015, pp.None, 2015, https://doi.org/10.1155/2015/329327
  5. KLAPS 재분석 자료를 활용한 집중호우의 3차원 분석 vol.26, pp.1, 2010, https://doi.org/10.14191/atmos.2016.26.1.097
  6. Approaches to radar reflectivity bias correction to improve rainfall estimation in Korea vol.9, pp.5, 2010, https://doi.org/10.5194/amt-9-2043-2016
  7. Changes in “hotter and wetter” events across China vol.134, pp.3, 2018, https://doi.org/10.1007/s00704-017-2344-x
  8. Spatiotemporal Change of Plum Rains in the Yangtze River Delta and Its Relation with EASM, ENSO, and PDO During the Period of 1960-2012 vol.10, pp.5, 2010, https://doi.org/10.3390/atmos10050258
  9. Classification of Rainfall Types Using Parsivel Disdrometer and S-Band Polarimetric Radar in Central Korea vol.12, pp.4, 2010, https://doi.org/10.3390/rs12040642
  10. Raindrop size distribution of rainfall system indirectly affected by Typhoon Kong-Rey (2018) passed through the southern parts of Korea vol.257, pp.None, 2021, https://doi.org/10.1016/j.atmosres.2021.105561