三维变分气象研究预报(WRF)模式与himawai -8卫星影像对帕朗卡拉亚暴雨的应用(以2018年4月27日为例)

N. Ayasha, Leny Octaviana Bota
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引用次数: 0

摘要

2018年4月27日,帕朗卡拉亚出现暴雨。根据Tjilik Riwut气象站的地面观测资料,降雨高峰发生在18-21 UTC之间,3小时内降雨量为54毫米。结果,第二天洪水泛滥了。本研究利用利用AMSU-A卫星热带物理套参数化方案和Himawari-8卫星IR-1数据同化的3DVar技术WRF模型,通过Python编程进行处理,探讨暴雨成因。结果表明,3DVar模式的WRF在总降水结果中代表性不足。然而,从WRF 3DVar模型来看,一些天气扰动显示了恶劣天气发生的潜力。在18和21 UTC的切变线和涡旋环流表明了这一趋势,而在15 - 18 UTC期间,气压时间序列以0.5 Mb的趋势下降。此外,Himawari-8卫星数据的云顶温度图显示,在18.20 UTC温度急剧下降至-61.4323,这支持了大雨过程。上述天气分析表明,WRF 3DVar对总降水结果的代表性不足,但对其他天气方面(切变线、涡动、气压)的代表性较好。因此,此次暴雨是由切变线和涡旋条件、云顶气压和低温造成的。
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The Utilization of Weather Research Forecasting (WRF) Model of 3DVar (Three Dimensional Variational) and Himawari-8 Satellite Imagery to the Heavy Rain in Palangkaraya (Case Study : April 27, 2018)
On April 27, 2018 heavy rain was occurred in Palangkaraya. Based on surface data observations at Tjilik Riwut Meteorological Station, the peak of rain occurred between 18-21 UTC, which 54 mm within 3 hours. As a result, the flood inundated on the following day. This research purposed to discover the cause of heavy rain used the WRF model of 3DVar technique that assimilated with AMSU-A satellite which used the tropical physic suite parameterization scheme and Himawari-8 Satellite (IR-1 data), processed by Python Programming. Based on the results, the WRF of the 3DVar model is not representative enough in total rainfall results. However, several weather disturbances show the potency for severe weather occurrence from WRF 3DVar modeling. These are indicated by the shear line and eddy circulation at 18 and 21 UTC, and the time series of air pressure decreases with a 0.5 Mb tendency between 15 to 18 UTC. Moreover, the cloud top temperature graph from Himawari-8 Satellite data shows a drastic reduction in temperature to -61.4323 at 18.20 UTC, which supports the heavy rain process. The weather analysis above show that WRF 3DVar is not representative enough for total rainfall result, but appropriate for other weather aspects (shear line, eddy, and air pressure). Therefore, the heavy rain is caused by shear line and eddy condition, air pressure and low temperature of the cloud top.
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