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논문 기본 정보

자료유형
학술저널
저자정보
저널정보
한국기상학회 대기 대기 Vol.19 No.1
발행연도
2009.3
수록면
67 - 78 (12page)

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초록· 키워드

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A strong negative correlation has been detected between the North Pacific Oscillation Index (NPI) and the Effective Drought Index (EDI) in May over Korea. In May of positive NPI year, anomalous patterns caused a drought in Korea as follows: the anomalous south-low, north?high low-level pressure patterns in the northeast and southeast of Korea have strengthened the anomalous northerlies to Korea. In addition, these anomalous northerlies have prevented western North Pacific (WNP) high from moving northward. As a result, anomalous descending flows have strengthened in the mid?latitude region in East Asia. In the WNP, the anomalous south?high, north?low sea surface temperature (SST) has been widely distributed, which has strengthened anomalous south?low, north?high low?level pressure patterns. These anomalous characteristics of pressure and SST patterns observed in May of positive NPI years have already been detected in previous winter (December?February) and early spring (March, April). In addition, the anomalous negative sea ice concentration in the North Pacific during two seasons has strengthened the anomalous anticyclonic circulation in the same region and in turn made a contribution to formation of anomalous south?low, north?high pressure patterns in May.

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Abstract
1. Introduction
2. Data and methodology
3. Correlation of EDI and NPI
4. Difference between positive and negative NPI years
5. Atmospheric environments during the preceding winter
6. Summary and conclusions
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