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Satellite-Based Assessment of Various Cloud Microphysics Schemes in Simulating Typhoon Hydrometeors

机译:基于卫星的卫星微妙计划模拟台风水质仪的评估

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The accurate simulation of typhoon hydrometeors remains a challenge. This study attempts to evaluate the performances of five microphysics schemes (MPSs) in the Weather Research and Forecasting (WRF) model in simulating the supertyphoon Neoguri in July 2014. The observed microwave brightness temperature, as well as retrieved data from the microwave radiometer imager (MWRI) onboard Chinese FY-3B satellite, are used to test hydrometeor simulations. In particular, two MWRI radiance indices, including the emission index (EI) and scattering index (SI), are used to assess the performance of five MPSs in simulating liquid and frozen hydrometeors, respectively. Overall, the WRF model can well reproduce the overall pattern of typhoon-produced precipitation, albeit with slightly overestimated precipitation in the inner rainband and underestimated precipitation in the stratiform rainband. Moreover, ice water paths (IWPs) from all five MPS simulations are higher than those estimated from MWRI retrieval in most areas, and the spatial pattern and values of IWP for the National Severe Storms Laboratory double-moment MPS (NSSL) are much closer to those for MWRI. The NSSL scheme reproduces a more realistic joint histogram distribution of SI and EI than other MPSs do, relative to the observation. Besides, the nonlinear Lucas–Kanade optical flow approach has been used to reflect the horizontal distribution of hydrometeors in the typhoon. The results show that the simulated EI and SI from the five MPSs show a systematic southwest bias of approximately about 10~20?km and significant intensity bias in the convection area. Further model sensitivity tests confirm that the NSSL scheme generates more realistic graupel and supercooled water close to the observations among all MPSs. The findings suggest that satellite measurements would be helpful to assess MPSs in numeric weather models, especially for hydrometeor distributions in the whole typhoon system.
机译:台风水质仪的准确仿真仍然是一个挑战。本研究试图评估20​​14年7月在模拟Supertyphoon Neoguri的天气研究和预测(WRF)模型中的五种微药物计划(MPS)的性能。观察到的微波亮度温度,以及从微波辐射计成像器中检索的数据( MWRI)船上中国FY-3B卫星,用于测试水流仪模拟。特别地,包括排放指数(EI)和散射指数(SI)的两个MWRI光索指数分别用于分别评估模拟液体和冷冻水中的5个MPS的性能。总的来说,WRF模型可以很好地再现雨风制作的沉淀的整体模式,尽管在内部雨带中略微高估的沉淀,层状雨筋中的低估沉淀。此外,来自所有五个MPS模拟的冰水路径(IWP)高于MWRI检索在大多数领域估计的冰水路径(IWP),以及全国严重风暴实验室双力MPS(NSSL)的IWP的空间模式和价值观更近那些为mwri。 NSSL方案再现比观察相对于其他MPS的Si和EI更真实的联合直方图分布。此外,非线性Lucas-Kanade光学流动方法已被用于反映台风中水流仪的水平分布。结果表明,来自五个MPS的模拟EI和SI显示出系统的西南偏置大约10〜20 km和对流区域的显着强度偏差。进一步的模型灵敏度测试确认NSSL方案会产生更现实的Graupel和过冷水,接近所有MPS中的观察。研究结果表明,卫星测量有助于评估数字天气模型中的MPS,特别是对于整个台风系统中的水流仪分布。

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