Turbulence analysis on the flight of Etihad airways in Bangka Island using the WRF case study May 4, 2016

Bayu Retna Tri Andari, N. J. Trilaksono, M. Munandar
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Abstract

Accurate weather forecasts should support the increase in safety of aviation operations in Indonesia. This weather forecast is needed, especially in detecting turbulence, considering that geographically Indonesia has effective solar radiation resulting in convective cloud formation. Convective clouds can trigger turbulence then produce disruption and even accidents on flights. This research uses a case study on the Etihad Airways flight on Bangka Island on May 4, 2016. At the time of the incident, there was turbulence at 39,000 feet altitude, and the aircraft did not enter the cloudy area. The Weather Research and Forecasting (WRF) model is used to simulate the turbulence in this study, which is downscaled up to 3 km with a microphysics parameterization of WRF Single Moment 6 Class (WSM6). The results were then verified using correlation and linear regression for temperature, wind direction, wind speed, and pattern resemblance between cloud fraction and the convective nuclei distribution. The turbulence is analyzed from the south-north and west-east vertical airflow. The turbulence spotted at 06.40 UTC when there is a quite strong updraft which can cause turbulence. The turbulence parameters used, such as the eddy dissipation rate (EDR) parameter, which has a value of 0.05 , Richardson number with a value of less than 0.25, and turbulence index (TI 1) with a maximum value of 4 x 10-7 s-2 found that turbulence was in a strong category. The turbulence that occurs in this study is identified as near cloud turbulence (NCT) event due to cloud formation observed in the west of the turbulence and intense updraft activity at the location of turbulence.
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2016年5月4日,阿提哈德航空公司在邦加岛的航班湍流分析,使用WRF案例研究
准确的天气预报应有助于提高印尼航空运营的安全性。这种天气预报是必要的,特别是在探测湍流时,考虑到印度尼西亚在地理上有有效的太阳辐射,导致对流云的形成。对流云会引发湍流,造成航班中断甚至事故。本研究以2016年5月4日阿提哈德航空在邦加岛的航班为例。事故发生时,飞机在39000英尺的高空出现了湍流,飞机没有进入多云区域。本文采用天气研究与预报(WRF)模式模拟湍流,并采用WRF单矩6级(WSM6)的微物理参数化,模拟尺度缩小至3 km。然后利用温度、风向、风速和云分与对流核分布的相似度的相关性和线性回归对结果进行验证。从南北垂直气流和西东垂直气流两方面分析了湍流。湍流发生在世界时6点40分,当时有一股很强的上升气流会引起湍流。采用涡耗散率(EDR)参数为0.05,理查德森数小于0.25,湍流指数(TI 1)最大值为4 × 10-7 s-2等湍流参数发现,湍流属于强类型。本研究中发生的湍流被确定为近云湍流(NCT)事件,因为在湍流的西部观测到云的形成和湍流位置强烈的上升气流活动。
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