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자료유형
학술저널
저자정보
저널정보
한국기상학회 Asia-Pacific Journal of Atmospheric Sciences Journal of the Korean Meteorological Society Vol.43 No.2
발행연도
2007.5
수록면
13 - 25 (13page)

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초록· 키워드

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The present study has analyzed the climatological characteristics of the tropical cyclones (TCs) made landfall on the Korean Peninsula (KP) during the period 1951 to 2004. Both the landfall frequency and the intensity of KP-landfall TCs have rapidly increased since the late 1980s. Especially, the frequency of TCs with an intensity greater than tropical storm remarkably have increased. The main landfalling track of KP-landfall TCs has also been changed. The TCs in the past mainly landed at the middle and northern regions of the west coast of the KP, but in recent years, the TCs have changed to land at the south coast and then pass through the east coast of the KP. That is, the main landfalling track tends to make a southeastward shift. The eastward shift was also discovered in the trend analyses of the recurving location of the KP-land-fall TCs and of the location of the western North Pacific High (WNPH). These kinds of eastward shifts are due to the southward advance of the upper-level trough of the mid-latitude and simultaneously the eastward expansion of the sub-tropical monsoon westerly. Meanwhile, the genesis location of KP-landfall TCs has been the farthest eastward only in the 2000s, but the trend toward an eastward shift has not been seen.

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Abstract
1. Introduction
2. Data and methodology
3. Changes in the KP-landfall TCs
4. Change in large-scale conditions in the western North Pacific
5. Summary and conclusions
Acknowledgements
REFERENCES

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