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Statistical analysis of wave parameters in the north coast of the Persian Gulf

机译:波斯湾北海岸波浪参数的统计分析

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In this study we have analysed wind and wave time series data resulting from hourly measurements on the sea surface in Bushehr, the northern part of the Persian Gulf, from 15 July to 4 August 2000. Wind speed (U_(10)) ranged from 0.34 to 10.38 m/s as alternating sea and land breezes. The lowest wind speed occurs at about midnight and the highest at around noon. The calculated autocorrelation of wind speed data shows that when the sea-land breeze is strong, the land-sea breeze is weak and vice versa. The significant wave height (H_s) varies between 0.10 to 1.02 m. The data of the present study reflects mostly the local waves or the sea waves. The calculated correlation between wind and wave parameters is rather weak, due to the continuous change in the wind direction. Wave height distribution follows the well-known Rayleigh distribution law. The cross correlation analyses between U_(10) and H_s reveal a time lag of 4h. Finally, we have shown that the time series of U_(10), H_s, and wave period are stationary. We have modeled these parameters by an auto regressive moving average (ARMA) and auto regressive integrated moving average (ARIMA) models.
机译:在这项研究中,我们分析了2000年7月15日至8月4日在波斯湾北部Bushehr海面每小时进行测量得出的风浪时间序列数据。风速(U_(10))的范围为0.34交替进行海风和陆风的速度达到10.38 m / s。最低风速发生在午夜左右,最高风速发生在中午左右。计算得到的风速数据的自相关表明,当海陆风较强时,海陆风较弱,反之亦然。有效波高(H_s)在0.10至1.02 m之间变化。本研究的数据主要反映了局部海浪或海浪。由于风向的不断变化,风与浪参数之间的计算相关性很弱。波高分布遵循众所周知的瑞利分布定律。 U_(10)和H_s之间的互相关分析显示了4h的时间滞后。最后,我们证明了U_(10),H_s和波浪周期的时间序列是固定的。我们通过自动回归移动平均值(ARMA)和自动回归综合移动平均值(ARIMA)模型对这些参数进行了建模。

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