首页> 外文期刊>Pure and Applied Geophysics >Role of Planetary Boundary Layer Processes in the Simulation of Tropical Cyclones Over the Bay of Bengal
【24h】

Role of Planetary Boundary Layer Processes in the Simulation of Tropical Cyclones Over the Bay of Bengal

机译:行星边界层过程在孟加拉湾热带旋风模拟中的作用

获取原文
获取原文并翻译 | 示例
       

摘要

The behaviour of planetary boundary layer (PBL) schemes initialized at different life stages of a tropical cyclone (TC) is studied by considering seven Bay of Bengal TC cases. In each TC case, the Advanced Research Weather Research and Forecasting (WRF-ARW) model is initialized at four life stages (depression to very severe cyclone storm) with National Center for Environmental Prediction (NCEP) Global analysis and integrated up to 96 h. A set of six PBL sensitivity experiments are conducted at four stages for all seven TC cases to analyse the impact of the model boundary layer in simulating the TC track and intensity parameters. The model-produced track, intensity and rainfall patterns are evaluated with the best track, intensity and gridded rainfall estimates obtained from the India Meteorological Department (IMD). The spatial and radius/height section simulated fields are evaluated with satellite retrievals. Results depict that the six PBL schemes during model initialization at different stages of a TC have produced sizable differences in the simulation of track and intensity parameters. The local and nonlocal schemes produced different results based on the TC stage at which the model is initialized. The results also suggest that if the model is initialized with a non-organized cyclonic vortex such as depression stage of the storm, PBL schemes exhibit high sensitivity and spread in terms of both track and intensity. While the spread between PBL schemes was significantly reduced and found close to the observed estimates when the model was initialized at the advanced stages of the TC. In addition, the local 1.5-order closure scheme simulated the storm parameters relatively better when the cyclone vortex was not well organized in the model's initial conditions, while the non-local and first-order closure schemes perform better with initial model conditions of a well-defined cyclonic vortex.
机译:通过考虑七叶的孟加拉特TC病例,研究了在热带气旋(TC)的不同寿命处初始化的行星边界层(PBL)方案。在每个TC案例中,高级研究天气研究和预测(WRF-ARW)模型在四个寿命(抑郁症到非常严重的旋风风暴)中初始化,具有国家环境预测中心(NCEP)全球分析,并集成了高达96小时。对于所有七个TC案例,在四个阶段进行了一组六个PBL敏感性实验,以分析模型边界层在模拟TC轨道和强度参数时的影响。模型产生的曲目,强度和降雨模式评估了从印度气象部门(IMD)获得的最佳轨道,强度和网格估计。空间和半径/高度剖面模拟字段是用卫星检索进行评估的。结果描绘了在TC的不同阶段的模型初始化期间的六个PBL方案在轨道和强度参数的模拟中产生了大量的差异。本地和非本地方案基于模型初始化的TC阶段产生不同的结果。结果还表明,如果模型用非有组织的循环涡流初始化,例如风暴的凹陷阶段,PBL方案表现出高灵敏度并在轨道和强度方面传播。虽然PBL方案之间的扩展显着减少,并且当模型在TC的高级阶段初始化时,靠近观察到的估计。此外,当旋风器涡旋在模型的初始条件下没有很好地组织时,本地1.5级闭合方案模拟了风暴参数,而非本地和一阶封闭方案在井的初始模型条件下表现更好 - 定义的循环涡旋。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号