Thermodynamic characteristics associated with localized torrential rainfall events in the southwest region of the Korean peninsula
详细信息    查看全文
  • 作者:Sueng-Pil Jung ; Tae-Yong Kwon ; Sang-Ok Han…
  • 关键词:Localized torrential rainfall ; thermodynamic characteristics ; convective cell life cycle ; radar rainfall ; radiosonde
  • 刊名:Asia-Pacific Journal of Atmospheric Sciences
  • 出版年:2015
  • 出版时间:August 2015
  • 年:2015
  • 卷:51
  • 期:3
  • 页码:229-237
  • 全文大小:1,181 KB
  • 参考文献:Barnolas, M., T. Rigo, and M. C. Llasat, 2010: Characteristics of 2-D convective structure in Catalonia (NE Spain): an analysis using radar data and GIS. Hydrol. Earth Syst. Sci., 14, 129-39.CrossRef
    Bunkers, M. J., J. S. Johnson, L. J. Czepyha, J. M. Grzywacz, B. A. Klimowski, and M. R. Hjelmfelt, 2006: An observational examination of long-lived supercells. Part II: Environmental conditions and forecasting. Wea. Forecasting, 21, 689-14.CrossRef
    Byers, H. R., and R. R. Braham ffixJr., 1949: The thunderstorm. Washington, D. C., U.S. Government Printing Office, 287 pp.
    Davies-Jones, R. P., D. Burgess, and M. Foster, 1990: Test of helicity as a tornado forcast parameter. Preprints, 16 th Conf. on Severe Local Storms, Kananaskis Park, AB, Canada. Amer. Meteor. Soc., 588-92.
    Djuric, D., 1994: Weather analysis. Prentice Hall, 304 pp.
    Eblen, L. H., J. W. Ladd, and T. M. Hicks, 1990: Severe thunderstorm forecasting. NOAA Tech. memo. NWS SR-130. National Weather Service Forecast Office, 42 pp.
    Fawbush, E. J., and R. C. Miller, 1954: The types of air masses in which North American tornadoes form. Bull. Amer. Meteor. Soc., 35, 154-65.
    Fujiwara, M., 1965: Raindrop-size distribution from individual storms. J. Atmos. Sci., 22, 585-91.CrossRef
    Han, L., S. X. Fu, L. F. Zhao, Y. Z. Zheng, H. Q. Wang, and Y. J. Lin, 2009: 3D Convective storm identification, tracking, and forecasting-An enhanced TITAN algorithm. J. Atmos. Oceanic Technol., 26, 719-32.CrossRef
    Hong, S.-Y., 2004: Comparison of heavy rainfall mechanisms in Korea and the Central US. J. Meteor. Soc. Japan., 5, 1469-479.CrossRef
    Im, E.-S., S.-R. In, and S.-O. Han, 2013: Numerical simulation of the heavy rainfall caused by a convection band over Korea: a case study on the comparison of WRF and CReSS. Natural Hazards, 69, 1681-695.CrossRef
    Johnson, J. T., P. L. Mackeen, A. Witt, E. D. Mitchell, G. Stumpf, M. D. Eilts, and K. W. Thomas, 1998: The storm cell identification and tracking algorithm: An enhanced WSR-88D algorithm. Wea. Forecasting, 13, 263-76.CrossRef
    Jung, S.-H., G. Lee, H.-W. Kim, and B. Kuk, 2011: Development of convective cell identification and tracking algorithm using 3-dimensional radar reflectivity fields. Atmosphere, 21, 243-56 (In Korean with English abstract).
    Jung, S.-P., T.-Y. Kwon, and S.-O. Han, 2014: Thermodynamic characteristics associated with localized torrential rainfall events in the Middle West region of Korean peninsula. Atmosphere, 24, 457-70 (In Korean with English abstract).CrossRef
    Kim, Y.-C., and S.-J. Ham, 2009: Heavy rainfall prediction using convective instability index. J. Korean Soc. for Aviation and Aeronautics, 17, 17-3 (In Korean with English abstract).
    Kirkpatrick, C., E. W. McCaul ffixJr., and C. Cohen, 2011: Sensitivity of simulated convective storms to environmental CAPE. Mon. Wea. Rev., 139, 3514-532.CrossRef
    Kwon, T.-Y., J.-S. Kim, and B.-G. Kim, 2013: Comparison of the properties of Yeongdong and Yeongseo heavy rain. Atmosphere, 23, 245-64 (In Korean with English abstract).CrossRef
    Lee, S.-M., and H.-R. Byun, 2011: Distribution of convective energy at upper level in South Korea and the possibility if artificial showery rain caused by activated CAPE. Theor. Appl. Climatol., 105, 537-51.CrossRef
    Lee, T.-Y., and Y.-H. Kim, 2007: Heavy precipitation systems over the Korean peninsula and their classification. J. Korean Meteorol. Soc., 43, 367-96.
    Marshall, J. S., and W. McK. Palmer, 1948: The distribution of raindrops with size. J. Meteor., 5, 165-66.CrossRef
    McCaul, E. W. ffixJr., and M. L. Weisman, 2001: The sensitivity of simulated supercell structure and intensity to variations in the shapes of environmental buoyancy and shear profiles. Mon. Wea. Rev., 129, 664-87.CrossRef
    Mecikalski, J. R., W. M. Mackenzie ffixJr., M. Koenig, and S. Muller, 2010: Cloud-top properties of growing cumulus prior to convective initiation as measured by meteosat second generation. Part I: Infrared fields. J. Appl. Meteor. Climatol., 49, 521-34.
    Meng, Z., D. Yan, and Y. Zhang, 2013: General feature of squall lines in east China. Mon. Wea. Rev., 141, 1629-647.CrossRef
    National Emergency Management Agency, 2014: Annual disaster report for 2013. 680 pp (In Korean).
    Park, C.-G., and T.-Y. Lee, 2008: Structure of mesoscale heavy precipitation systems originated from the changma front. Atmosphere, 18, 317-38 (In Korean with English abstract).
    Rasmussen, E. N., and D. O. Blanchard, 1998: A baseline climatology of sounding-derived supercell and tornado forecasting parameters. Wea. Forecasting, 13, 1148-164.CrossRef
    Suk, M.-K., K.-H. Chang, J.-W. Cha, and K.-E. Kim, 2013: Operational real-time adjustment of radar rainfall estimation over the South Korea region. J. Meteor. Soc. Japan, 91, 545-54.CrossRef
    Schultz, C. J. and M. A. Askelson, 2012: Vertical variations of boundary layer potential buoyancy in tornadic and nontornadic n
  • 作者单位:Sueng-Pil Jung (1) (2)
    Tae-Yong Kwon (2)
    Sang-Ok Han (1)
    Jong-Hyeok Jeong (1)
    JaeKwan Shim (1)
    Byoung-Choel Choi (1)

    1. High-impact Weather Research Center, Observation Research Division, National Institute of Meteorological Research, KMA, Gangneung, Korea
    2. Department of Atmospheric and Environmental Sciences, Gangneung-Wonju National University, 7 Jukheon-gil, Gangneung-si, Gangwon-do, 210-702, Korea
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:Earth sciences
    Geophysics and Geodesy
    Meteorology and Climatology
  • 出版者:Korean Meteorological Society, co-published with Springer
  • ISSN:1976-7951
文摘
This study uses observational data from radar and radiosonde to investigate the thermodynamic conditions related to localized torrential rainfall (LTR) in the southwest region of the Korean peninsula. Three criteria were defined for selecting LTR events: 1) hourly rainfall exceeding 30 mm h? recorded at any of the automated synoptic observing systems (ASOS) around Gwangju, 2) an area of rainfall at > 1 mm h? (as estimated from radar rain rate) of less than 20,000 km2, and 3) clearly defined stages of genesis and dissipation in a group of rain cells (> 10 mm h?) with a duration lasting less than 24 hours. As a result, 10 cases were selected from the summer season (June-August) over the last decade (2004-2013). Results showed all cases occurred during the afternoon hours and that the duration and maximum rain area of convective cells (> 30 mm h?) was less than 6 hours and smaller than 700 km2, respectively. The majority of cases showed the following thermodynamic characteristics: 1) strong convective available potential energy (CAPE > 1,500 J kg?) related to surface heating, 2) weak (or no) convective inhibition (CIN < 50 J kg?), 3) adequate moisture and total precipitable water (TPW ?55 mm), and 4) values of storm relative helicity (SRH) of less than 10 m2 s?. The area of rainfall (700 km2) and the duration (6 h) in this experiment were relatively small and short, respectively, compared to those in a previous study in the middle-west region of Korea (1,000 km2, 9 h), but a higher CAPE (1,500 J kg?) and lower SRH (10 m2 s?) were involved in this study than in the former (800 J kg?, 120 m2 s?). Key words Localized torrential rainfall thermodynamic characteristics convective cell life cycle radar rainfall radiosonde

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700