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Impact of ocean coupling on typhoon prediction in high-resolution nonhydrostatic global model

机译:海洋耦合对高分辨率非静水全球模式中台风预报的影响

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Accurate prediction of intensity and track of typhoon is crucial to mitigate typhoon disasters. To improve typhoon forecast, the “Global 7-km mesh nonhydrostatic model inter-comparison project for improving typhoon forecast (TYMIP-G7)” has been conducted under the JAMSTEC Earth Simulator Strategic Project with Special Support. In the project, ensemble of the 5-day typhoon forecast experiments in September and October 2013 were conducted by using three nonhydrostatic global atmospheric models. Preliminary results indicate that the nonhydrostatic models significantly improve the forecast skill in terms of typhoon intensity. However, the atmospheric models used in TYMIP-G7 are not fully coupled with ocean. This study aims to investigate the impact of ocean coupling on typhoon simulation by using a nonhydrostatic global ocean-atmosphere coupled general circulation model. It was found that the forecast error of typhoon intensity ranged from - 10 hPa to 10 hPa at the forecast time of 60 hours in the coupled model. We also found that there is no marked difference in the modeled typhoon intensity at the forecast lead time of 36 hours between the coupled model and standalone atmospheric model; however, the typhoon intensity was weakened after the forecast lead time of 36 hours in the coupled model compared to the standalone model. On the other hand, the forecast error of typhoon track was not changed by ocean coupling, indicating that large scale atmospheric circulations were not changed by ocean coupling in the 5-day simulation.
机译:准确预测台风的强度和轨迹对于减轻台风灾害至关重要。为了改善台风预报,在“ JAMSTEC地球模拟器战略计划”的特别支持下,开展了“全球7公里网状非静水模型用于提高台风预报的比对项目(TYMIP-G7)”。在该项目中,通过使用三个非静水全球大气模型进行了2013年9月和2013年10月的5天台风预报实验的合奏。初步结果表明,非静水模型在台风强度方面显着提高了预报技能。但是,TYMIP-G7中使用的大气模型并未完全与海洋耦合。本研究旨在通过使用非静水全球海洋-大气耦合总环流模型研究海洋耦合对台风模拟的影响。在耦合模型中,在60小时的预测时间发现台风强度的预测误差在-10 hPa至10 hPa的范围内。我们还发现,在耦合模式和独立大气模式之间,在预测的36小时提前期,台风强度模拟没有显着差异。但是,与独立模型相比,耦合模型的预测提前时间为36小时后,台风强度减弱。另一方面,台风路径的预报误差没有因海洋耦合而改变,这表明在5天的模拟中,大尺度大气环流没有因海洋耦合而改变。

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