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Spectral analysis of wind field in the Indian Ocean

机译:印度洋风场的频谱分析

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摘要

To study the variability in wind fields over the Indian Ocean, we used ERA INTERIM daily winds for the period 1979-2012. In order to analyse the temporal variation of wind field, we partitioned the whole Indian Ocean into 6 zones based on spatial inhomogeneity in the analysed wind fields. Spectral analysis of the time series (extracted at the centre of each zone) was performed using the auto-regression analysis based on the Yule-Walker equations. and it confirms that universality of the spectral shaps Frequency spectra show distinct annual variations at all zones; semi-annual variations are observed in the Arabian Sea (Z1) and the Bay of Bengal (Z2) due to the seasonal changes and gradually it disappears from equatorial region (Z3) to southern Indian Ocean (Z6). Also, we observe local maxima at the scale of 1 and 0.5 days(-1). The characteristic shape of the spectrum was obtained at two different powers of the frequencies. Decay rate and variance at all zones are analysed. The decay rate varies almost linearly as a function of zones Z1 to Z6. Trend of the variance in low frequency range is linear whereas, in high frequency range is exponential. The variance is large in the storm track region. It is found that over the range of frequencies, wind field is independent and is increasing along the zones Z1 to Z6. Latitudinal dependency is clearly observed in both spectral slopes and variances.
机译:为了研究印度洋上风场的变化,我们使用了ERA INTERIM 1979-2012年期间的日风。为了分析风场的时间变化,我们基于分析风场中的空间不均匀性将整个印度洋划分为6个区域。使用基于Yule-Walker方程的自动回归分析对时间序列(在每个区域的中心提取)进行光谱分析。它证实了频谱整形的普遍性频谱在所有区域都显示出明显的年度变化;由于季节变化,在阿拉伯海(Z1)和孟加拉湾(Z2)观察到半年变化,并从赤道区(Z3)到印度洋南部(Z6)逐渐消失。此外,我们在1天和0.5天(-1)的规模上观察到局部最大值。频谱的特征形状是在两个不同频率的功率下获得的。分析所有区域的衰减率和方差。衰减率几乎随区域Z1至Z6线性变化。低频范围的变化趋势是线性的,而高频范围的变化是指数的。在风暴轨迹区域中,方差很大。发现在整个频率范围内,风场是独立的,并且沿着区域Z1至Z6不断增加。在频谱斜率和方差中都清楚地观察到纬度依赖性。

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