An FFT-Based Method for Wave Decomposition from Wave and Tide Monitoring Using A01NYUB Sensor

Sekar Adiningsih, Y. N. Fadlilah, Rizki Taqwa Putranto, Syifa Agfanita, Salmaa Bayrus, Rossi Nur Iriani, Moses Wicaksono, S. Ikhtiarino, S. Wulandari, Yustinus Adyaksa, C. B. Petrova, Satria Ginanjar, A. Wirasatriya, R. Widiaratih, D. Sugianto, Kunarso Kunarso, R. Susanto
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Abstract

Monitoring Sea level to obtain tide and wave values using acoustic sensors has the potential to be influenced by other factors. This causes the measurement results to have noise that can affect the quality of the resulting monitoring data. This study aims to decompose the monitoring results of the time series sea level data, to show the recorded wave variations. This study is located in Teluk Awur, Jepara, Indonesia. Sea level data was recorded for ten days using the A01NYUB ultrasonic sensor starting on November 4, 2022, to November 13, 2022. The results of the recording data from the A01NYUB sensor were decomposed using Fast Fourier Transform (FFT) and Continuous Wavelet Transform (CWT) based on the classification of the wave period. The results of the decomposition of sea level data from the sensor show that there are several classifications of waves with different periods. There are Ordinary Gravity Waves with a period of 15s-30s and an amplitude of ~1 cm; with Infragravity Waves a period of 30 s – 5 m and an amplitude of ~8.5 cm; are Long Period Waves with a period of 5min – 12h and an amplitude of ~60 cm; Ordinary Tide Waves with a period of 12h – 24h and an amplitude of ~10 cm; and Trans tidal Waves with a period of 12h – more and an amplitude of ~7.9 cm. The monitoring data were also adjusted to the MSL datum. The waters of Jepara have tidal characteristics, namely tidal asymmetry.The tides in Teluk Awur are mixed tides prevailing semi-diurnal. The A01NYUB ultrasonic sensor can record wave data with the lowest period which is Ordinary Gravity Waves and the highest period which is Trans Tidal Waves.
基于fft的A01NYUB波潮监测波浪分解方法
利用声传感器监测海平面以获取潮汐和波浪值可能会受到其他因素的影响。这会导致测量结果有噪声,从而影响所得到的监测数据的质量。本研究旨在对时间序列海平面数据的监测结果进行分解,以显示记录的海浪变化。本研究位于印度尼西亚Jepara的Teluk Awur。从2022年11月4日至11月13日,使用A01NYUB超声波传感器记录了10天的海平面数据。基于波周期分类,对A01NYUB传感器的记录数据进行快速傅里叶变换(FFT)和连续小波变换(CWT)分解。对传感器海平面数据的分解结果表明,不同周期的波浪有几种类型。有周期为15 ~ 30秒、振幅为~1 cm的普通重力波;次重力波周期为30 s ~ 5 m,振幅为~8.5 cm;为长周期波,周期为5min ~ 12h,振幅为~ 60cm;周期为12h ~ 24h,振幅为~ 10cm的普通潮汐波;周期为12h以上,振幅为~7.9 cm的跨潮波。监测数据也调整为MSL基准。耶帕拉水域具有潮汐特征,即潮汐不对称。泰鲁克阿乌尔的潮汐是半昼夜的混合潮汐。A01NYUB超声传感器可以记录最低周期为普通重力波,最高周期为反潮汐波的波浪数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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