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Sensitivity of Typhoon Vamei (2001) Simulation to Planetary Boundary Layer Parameterization Using PSU/NCAR MM5

机译:使用PSU / NCAR MM5的台风Vamei(2001)模拟对行星边界层参数化的敏感性

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This paper investigates the sensitivity of the numerical simulations of a near equatorial Typhoon Vamei (2001) to various planetary boundary layer (PBL) parameterization schemes in the Pennsylvania State University (PSU)/National Centre for Atmospheric Research (NCAR) non-hydrostatic mesoscale model (MM5). The numerical simulations are conducted on two domains at 45 and 15 km grids nested in a one-way fashion. Four different PBL parameterization schemes including the Blackadar (BLK) scheme, the Burk-Thompson (BURKT) scheme, the NCEP Eta model scheme and the NCEP medium range forecast (MRF) model scheme are investigated. Results indicate that the intensity and propagation track of the simulated near equatorial typhoon system is not very sensitive to the different PBL treatments. The simulated minimum central pressures and the maximum surface wind speeds differ by only 5-6 hPa and 6-8 ms ?1, respectively. Larger variations between the simulations occur during the weakening phase of the typhoon system. While all schemes simulated the typhoon with reasonable accuracy, the ETA scheme produces the strongest storm intensity with the largest heat exchanges over the marine environment and the highest warm moisture air content in the PBL around the core of the storm.
机译:本文研究了宾夕法尼亚州立大学(PSU)/国家大气研究中心(NCAR)非静水中尺度模型中近赤道台风Vamei(2001)数值模拟对各种行星边界层(PBL)参数化方案的敏感性(MM5)。在以单向方式嵌套的45 km和15 km网格的两个域上进行了数值模拟。研究了四种不同的PBL参数化方案,包括Blackadar(BLK)方案,Burk-Thompson(BURKT)方案,NCEP Eta模型方案和NCEP中程预报(MRF)模型方案。结果表明,模拟的近赤道台风系统的强度和传播轨迹对不同的PBL处理不是很敏感。模拟的最小中心压力和最大表面风速分别仅相差5-6 hPa和6-8 ms?1。模拟之间的较大变化发生在台风系统的弱化阶段。虽然所有方案都以合理的精度模拟了台风,但ETA方案产生了最强的风暴强度,在海洋环境中具有最大的热交换,并且在风暴中心附近的PBL中具有最高的暖湿空气含量。

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