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자료유형
학술저널
저자정보
저널정보
한국기상학회 대기 대기 Vol.17 No.4
발행연도
2007.12
수록면
393 - 405 (13page)

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Simulation results of WRF for the case of typhoon ‘Rusa’ were analyzed, comparing with observed data especially for the Gangneung area around to examine its ability in numerical simulation. From the hourly precipitation time series, two peaks were found at Gangneung and Daegwallyeong, while only one peak was found from those of inland regions else. Especially, for the Yeongdong region, the first peak was directly related to spiral bands generated in front of the typhoon. Convective cells that were developed within the spiral bands moved to the eastern coastal area from the sea so that local heavy rainfall occurred in the Yeongdong region. The second peak was mainly related to the accompanying rain band of typhoon itself, topographic effect and the convergence near Gangneung area. Precipitation in Gangneung was simulated as much as about 30% of observed one. The main reason of this result came from a poor representation of wind directions in Gangneung area of WRF model. Observed wind direction was northwesterly but simulated one was nearly easterly in the area. This might shift a local heavy rainfall area downstream to the mountain area rather than the coastal area.

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Abstract
1. 서론
2. 관측자료 분석
3. 수치모델 및 모의 결과
4. 종합 및 결론
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