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Physical and dynamic factors that drove the heavy rainfall event over the middle Korean Peninsula on 26-27 July 2011

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Abstract

This study used an observational analysis and a numerical model to investigate the heavy rainfall event that occurred on 26-27 July 2011 over the middle Korean Peninsula. Radar observations revealed a significant transition in the echo pattern, with strong convective systems along the coasts of southern Hwanghae-do (HHD) and Gyeonggi-do (0600-1200 UTC 26 July, stage 1), a medium-sized SW-NE precipitation band over the middle Korean Peninsula and major convective systems in the west (1500-2200 UTC, stage 2), and a narrow convective band from Gyeonggi Bay to the Seoul metropolitan area (2200 UTC 26-0100 UTC 27 July, stage 3). This study focused on the development of heavy precipitation systems during stages 1 and 2. A mesoscale ridge and trough developed over the middle peninsula at approximately 0600 UTC on 26 July and persisted throughout the first 2 stages. Both the observation and the numerical simulation suggest that a cold pool, which induced the mesoscale ridge, developed over the inland HHD in response to evaporative cooling of rain water. The outflow associated with the cold pool was found to trigger the strong convective systems along the southern coast of HHD in stage 1. The lifting of air in the precipitation band of stage 2 was mainly caused by convergence ahead of the strong low-level southwesterly flow. The numerical simulations indicated that the terrain over the Korean Peninsula contributed to the enhancement of the heavy rainfall primarily through its blocking effects on oncoming southwesterly airflow at low levels.

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References

  • Bluestein, H. B., and M. H. Jain, 1985: Formation of mesoscale lines of precipitation: severe squall lines in Oklahoma during the spring. J. Atmos. Sci., 42, 1711–1732, doi:10.1175/1520-0469(1985)042<1711: FOMLOP>2.0.CO;2.

    Article  Google Scholar 

  • Chen, C.-S., W.-S. Chen, and Z. Deng, 1991: A study of a mountaingenerated precipitation system in Northern Taiwan during TAMEX IOP 8. Mon. Wea. Rev., 119, 2574–2607, doi:10.1175/1520-0493(1991)119<2574:ASOAMG>2.0.CO;2.

    Article  Google Scholar 

  • Chen, Y.-L., and J. Li, 1995: Characteristics of surface air-flow and pressure patterns over the island of Taiwan during Tamex. Mon. Wea. Rev., 123, 695–716, doi:10.1175/1520-0493(1995)123<0695:COSAAP>2.0. CO;2.

    Article  Google Scholar 

  • Choi, H.-Y., J.-H. Ha, D.-K. Lee, and Y.-H. Kuo, 2011: Analysis and simulation of mesoscale convective systems accompanying heavy rainfall: the Goyang case. Asia-Pac. J. Atmos. Sci., 47, 265–279, doi: 10.1007/s13143-011-0015-x.

    Article  Google Scholar 

  • Hong, S.-Y., 2004: Comparison of heavy rainfall mechanisms in Korea and the central US.J. Meteor. Soc. Japan, 82, 1469–1479, doi:10.2151/jmsj. 2004.1469

    Article  Google Scholar 

  • Hong, S.-Y., and J.-O. J. Lim, 2006: The WRF single-moment 6-class microphysics scheme (WSM6). J. Korean Meteor. Soc., 42, 129–151.

    Google Scholar 

  • Iacono, M. J., J. S. Delamere, E. J. Mlawer, M. W. Shephard, S. A. Clough, and W. D. Collins, 2008: Radiative forcing by long-lived greenhouse gases: calculations with the AER radiative transfer models. J. Geophys. Res., 113, D13103, doi:10.1029/2008JD009944.

    Article  Google Scholar 

  • Janji, Z. I., 1994: The step-mountain eta coordinate model: Further developments of the convection, viscous sublayer, and turbulence closure schemes. Mon. Wea. Rev., 122, 927–945, doi:10.1175/1520-0493(1994)122<0927:TSMECM>2.0.CO;2.

    Article  Google Scholar 

  • Jeong, J.-H., D.-I. Lee, and C.-C. Wang, 2016: Impact of Cold Pool on Mesoscale Convective System Produced Extreme Rainfall over southeastern South Korea: 7 July 2009. Mon. Wea. Rev., 144, 3985–4006, doi:10.1175/MWR-D-16-0131.1.

    Article  Google Scholar 

  • Kain, J. S., 2004: The Kain-Fritsch convective parameterization: An update. J. Appl. Meteorol., 43, 170–181, doi:10.1175/1520-0450(2004) 043<0170:TKCPAU>2.0.CO;2.

    Article  Google Scholar 

  • Kato, T., 1998: Numerical simulation of the band-shaped torrential rain observed over southern Kyushu, Japan on 1 August 1993. J. Meteor. Soc. Japan, 76, 97–128.

    Google Scholar 

  • Kim, D.-K., and H.-y. Chun, 2000: A numerical study of the orographic effects associated with a heavy rainfall event. J. Korean Meteor. Soc., 36, 441–454 (in Korean with English abstract).

    Google Scholar 

  • Kim, H. W., and D. K. Lee, 2006: An observational study of mesoscale convective systems with heavy rainfall over the Korean Peninsula. Wea. Forecasting, 21, 125–148, doi:10.1175/WAF912.1.

    Article  Google Scholar 

  • KMA, 2012: Learning from the cases in recent 20 years - top ten heavy rainfall events. Korea Meteorological Administration, Seoul, 47 pp (in Korean).

    Google Scholar 

  • Lee, D.-K., J.-G. Park, and J.-W. Kim, 2008: Heavy rainfall events lasting 18 days from July 31 to August 17, 1998, over Korea. J. Meteor. Soc. Japan, 86, 313–333, doi:10.2151/jmsj.86.313.

    Article  Google Scholar 

  • Lee, J.-T., D.-I. Lee, C.-H. You, H. Uyeda, Y.-C. Liou, and I.-S. Han, 2014a: Dual-Doppler radar analysis of a near-shore line-shaped convective system on 27 July 2011, Korea: a case study. Tellus, 66, 23453, doi:10.3402/tellusa.v66.23453.

    Google Scholar 

  • Lee, J. G., and Y. J. Kim, 2009: A numerical case study examining the orographic effect of the northern mountain complex on snowfall distribution over the Yeongdong region. Atmosphere, 19, 345–370 (in Korean with English abstract).

    Google Scholar 

  • Lee, K.-O., H. Uyeda, and D.-I. Lee, 2014b: Effect of an isolated elliptical terrain (Jeju Island) on rainfall enhancement in a moist environment. Tellus, 66, 20484, doi:10.3402/tellusa.v66.20484.

    Google Scholar 

  • Lee, T.-Y., and Y.-y. Park, 1996: Formation of a mesoscale trough over the Korean peninsula during an excursion of the Siberian High. J. Meteor. Soc. Japan, 74, 299–323.

    Google Scholar 

  • Lee, T.-Y., and Y.-H. Kim, 2007: Heavy precipitation systems over the Korean peninsula and their classification. J. Korean Meteor. Soc., 43, 367–396.

    Google Scholar 

  • Lee, T.-Y., Y.-y. Park, and Y.-H. Kim, 1998a: A numerical modeling study of heavy rainfall development over the Changma front. Proc., International Conference on Monsoon and Hydrologic Cycle, Kyongju, Korea, 72–75.

    Google Scholar 

  • Lee, T.-Y., Y.-y. Park, and Y.-L. Lin, 1998b: A numerical modeling study of mesoscale cyclogenesis to the east of the Korean peninsula. Mon. Wea. Rev., 126, 2305–2329, doi:10.1175/1520-0493(1998)126<2305:ANMSOM> 2.0.CO;2.

    Article  Google Scholar 

  • Lim, E.-H., and T.-y. Lee, 1994: Two-dimensional numerical study of the terrain effects on the development of cloud and precipitation for the middle part of Korea. J. Korean Meteoro. Soc., 30, 565–582 (in Korean with English abstract).

    Google Scholar 

  • Nagata, M., 1991: Further numerical study on the formation of the convergent cloud band over the Japan Sea in winter. J. Meteor. Soc. Japan, 69, 419–428.

    Google Scholar 

  • NEMA, 2012: Annual disaster report for 2011. National Emergency Management Agency, Seoul, 973 pp (in Korean).

    Google Scholar 

  • Pierrehumbert, R. T., 1984: Linear results on the barrier effects of mesoscale mountains. J. Atmos. Sci., 41, 1356–1367, doi:10.1175/1520-0469(1984)041<1356:LROTBE>2.0.CO;2.

    Article  Google Scholar 

  • Saha, S., and Coauthors, 2010: The NCEP climate forecast system reanalysis. Bull. Amer. Meteor. Soc., 91, 1015–1057, doi:10.1175/2010-BAMS3001.1.

    Article  Google Scholar 

  • Seo, K.-H., and D.-K. Lee, 1996: Analysis and simulation of orographic rain in the middle part of the Korean Peninsula. Asia-Pac. J. Atmos. Sci., 32, 511–533 (in Korean with English abstract).

    Google Scholar 

  • Shin, C.-S., and T.-y. Lee, 2005: Development mechanisms for the heavy rainfalls of 6-7 August 2002 over the middle of the Korean Peninsula. J. Meteor. Soc. Japan, 83, 683–709, doi:10.2151/jmsj.83.683.

    Article  Google Scholar 

  • Shin, U., and T.-y. Lee, 2015: Origin, evolution and structure of mesoalpha-scale lows associated with cloud clusters and heavy rainfall over the Korean peninsula. Asia-Pac. J. Atmos. Sci., 51, 259–274, doi:10. 1007/s13143-015-0076-3.

    Article  Google Scholar 

  • Skamarock, W. C., J. B. Klemp, J. Dudhia, D. O. Gill, D. M. Barker, M. G. Duda, X. Y. Huang, W. Wang, and J. G. Powers, 2008: A description of the advanced research WRF V.3. NCAR Tech. Note NCAR/TN-475+STR, 113 pp.

    Google Scholar 

  • Smith, R. B., 1982: Synoptic observations and theory of orographically disturbed wind and pressure. J. Atmos. Sci., 39, 60–70, doi:10.1175/1520-0469(1982)039<0060:SOATOO>2.0.CO;2.

    Article  Google Scholar 

  • Tsuguti, H., and T. Kato, 2014: Contributing factors of the heavy rainfall event at Amami-Oshima Island, Japan, on 20 October 2010. J. Meteor. Soc. Japan, 92, 163–183, doi:10.2151/jmsj.2014-202.

    Article  Google Scholar 

  • Wang, C.-C., G. T.-J. Chen, T.-C. Chen, and K. Tsuboki, 2005: A numerical study on the effects of Taiwan topography on a convective line during the mei-yu season. Mon. Wea. Rev., 133, 3217–3242, doi: 10.1175/MWR3028.1.

    Article  Google Scholar 

  • Yamada, H., B. Geng, K. K. Reddy, H. Uyeda, and Y. Fujiyoshi, 2003: Three-dimensional structure of a mesoscale convective system in a Baiu-frontal depression generated in the downstream region of the Yangtze river. J. Meteor. Soc. Japan, 81, 1243–1271, doi:10.2151/jmsj. 81.1243.

    Article  Google Scholar 

  • Yoshizaki, M., T. Kato, Y. Tanaka, H. Takayama, Y. Shoji, H. Seko, K. Arao, and K. Manabe, 2000: Analytical and numerical study of the 26 June 1998 orographic rainband observed in western Kyushu, Japan. J. Meteor. Soc. Japan, 78, 835–856.

    Google Scholar 

  • Zhang, Y., L. F. Zhang, C. M. Wang, Y. Q. Xie, and J. Xiang, 2014: Mechanism of a torrential rainstorm that occurred to the west of a Meiyu frontal low. Asia-Pac. J. Atmos. Sci., 50, 437–452, doi:10.1007/s13143-014-0034-5.

    Article  Google Scholar 

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Correspondence to Wonsu Kim.

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Lee, JY., Kim, W. & Lee, TY. Physical and dynamic factors that drove the heavy rainfall event over the middle Korean Peninsula on 26-27 July 2011. Asia-Pacific J Atmos Sci 53, 101–120 (2017). https://doi.org/10.1007/s13143-017-0009-4

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  • DOI: https://doi.org/10.1007/s13143-017-0009-4

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