Abstract
This study carried out a comparative analysis of the changes in tropical cyclone (TC) genesis, TC track, and TC intensity focusing on TCs that affected the Korean peninsula (KP) according to three evolutionary patterns (prolonged, abrupt and symmetric-decay) of the abnormal sea surface temperature in the Central-Pacific (CP) region. As a result of the analysis, the activity pattern of TCs was found to vary depending on the evolution patterns of the CP El Niño, and such changes appeared to result in clear variations in the regional rainfall in Korea. In the prolonged-decaying and symmetric-decaying years, the KP received considerable TC rainfall. On the other hand, in abrupt-decaying years, it was subtly affected by the TC rainfall. Although rather limited conditions and relatively short observation data were used to analyze the effects of the evolution pattern of the CP El Niño on TCs, the results can be used to quantitatively identify the spatial features of TCs affecting the KP. These results are expected to be helpful in managing the disaster risks in vulnerable areas, including plans to secure stable water resources in the basin, and in establishing effective and active measures to cope with natural disasters by extreme events over the KP.
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Acknowledgments
This CRI work was supported by the National Research Foundation of Korea (NRF) grant funded by the Korea government (2012R1A1A2005304) and also funded by The Korea Meteorological Administration Research and Development Program under grant CATER 2012-3100 (Development of Drought Outlook. Response Techniques on Korea and East Asia). The authors thank the editor and the two anonymous reviewers for their constructive comments and valuable suggestions, which helped us to improve the manuscript.
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Son, CY., Kim, JS., Moon, YI. et al. Characteristics of tropical cyclone-induced precipitation over the Korean River basins according to three evolution patterns of the Central-Pacific El Niño. Stoch Environ Res Risk Assess 28, 1147–1156 (2014). https://doi.org/10.1007/s00477-013-0804-0
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DOI: https://doi.org/10.1007/s00477-013-0804-0