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高分辨率海溫數(shù)據(jù)對1810號臺風“安比”WRF數(shù)值模擬的影響

單位：國家海洋環(huán)境預報中心, 北京 100081

分類號：P444

出版年·卷·期（頁碼）：2022·39·第一期（80-90）

摘要：

采用美國國家環(huán)境預報中心高空間分辨率再分析海溫資料和中國國家海洋環(huán)境預報中心提供的逐小時全球高時間分辨率海溫數(shù)據(jù)，通過WRF模式對2018年10號臺風"安比"（1810）進行數(shù)值模擬，結合臺風動力和熱力條件分析結果表明：海溫分布與位渦強度具有良好的一致性；海溫通過影響臺風內部垂直運動帶來的潛熱釋放決定對臺風強度的改變，高分辨率的海溫數(shù)據(jù)對臺風數(shù)值模擬有一定影響。

Based on the sea surface temperature (SST) reanalysis data with high spatial resolution of the National Centers for Environmental Prediction and the hourly SST data with global coverage of the National Marine Environmental Forecasting Center, the Weather Research and Forecasting model is used to simulate typhoon "Ampil" (1810) in this paper. Taking the analysis results of typhoon dynamic and thermal conditions into consideration, it is found that the SST distribution is in good agreement with the intensity of the potential vorticity, and SST determines the variation of typhoon intensity by affecting the latent heat release caused by the vertical movement within the typhoon. Therefore, high-resolution SST data has a certain impact on the numerical simulation of typhoon.

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