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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 30, issue 8
Ann. Geophys., 30, 1235–1248, 2012
https://doi.org/10.5194/angeo-30-1235-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 30, 1235–1248, 2012
https://doi.org/10.5194/angeo-30-1235-2012
© Author(s) 2012. This work is distributed under
the Creative Commons Attribution 3.0 License.

Regular paper 22 Aug 2012

Regular paper | 22 Aug 2012

Environment and morphology of mesoscale convective systems associated with the Changma front during 9–10 July 2007

J.-H. Jeong1, D.-I. Lee1, C.-C. Wang2, S.-M. Jang1, C.-H. You3, and M. Jang4 J.-H. Jeong et al.
  • 1Department of Environmental Atmospheric Sciences, Pukyong National University, Busan, South Korea
  • 2Department of Earth Sciences, National Taiwan Normal University, Taipei, Taiwan
  • 3Radar Analysis Division, Weather Radar Center, KMA,Seoul, South Korea
  • 4Applied Meteorology R&D Center, Weatherlink INC., SungNam, South Korea

Abstract. To understand the different environment and morphology for heavy rainfall during 9–10 July 2007, over the Korean Peninsula, mesoscale convective systems (MCSs) that accompanied the Changma front in two different regions were investigated. The sub-synoptic conditions were analysed using mesoscale analysis data (MANAL), reanalysis data, weather charts and Multi-functional Transport Satellite (MTSAT-IR) data. Dual-Doppler radar observations were used to analyse the wind fields within the precipitation systems. During both the case periods, the surface low-pressure field intensified and moved northeastward along the Changma front. A low-level warm front gradually formed with an east-west orientation, and the cold front near the low pressure was aligned from northeast to southwest.

The northern convective systems (meso-α-scale) were embedded within an area of stratiform cloud north of the warm front. The development of low-level pressure resulted in horizontal and vertical wind shear due to cyclonic circulation. The wind direction was apparently different across the warm front. In addition, the southeasterly flow (below 4 km) played an important role in generating new convective cells behind the prevailing convective cell. Each isolated southern convective cell (meso-β-scale) moved along the line ahead of the cold front within the prefrontal warm sector. These convective cells developed when a strong southwesterly low-level jet (LLJ) intensified and moisture was deeply advected into the sloping frontal zone. A high equivalent potential temperature region transported warm moist air in a strong southwesterly flow, where the convectively unstable air led to updraft and downdraft with a strong reflectivity core.

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