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Wavelet Analysis for Internal Wave Detection in ERS SARand ASTER Image Data

机译:ERS SAR和ASTER图像数据内波检测的小波分析

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On this paper, wavelet analysis has been used for internal wave detection in ERS SAR and ASTER image data over Tsushima strait, southwest of Japan, during 1993-2004 period. Various wavelet transforms, e.g. Haar wavelet, Symlet wavelet, Biorthogonal wavelet, Coif wavelet and Daubechies wavelet, are tested comparably with different level of synthesize image on horizontal, diagonal, and vertical detail, and approximation to study the internal wave characteristic in image.Internal wave features were detected as elongated pattern in image with higher wavelet coefficient (>36) than sea surface (<10) on horizontal and vertical detail coefficient of image transforms at level 2-5. The decomposition image shows thetendency that the decomposition of internal wave feature using wavelet transform tends to follow the wavelet function. This may reduced the height of leading wave. Smoother result of internal wave shape can be formed using higher scale resolutionof image at level 5 and higher number of vanishing moments such as Daubechies wavelet-db5), Symlet wavelet-sym5, and Discrete Meyer wavelet. The compactly supported wavelet function with orthogonal basis with scale function and FIR filter, such as discrete Meyer function is proposed for smoothness of feature, space save coding, and to avoid depashing in image.So far, the detection processes were performed well on the internal waves data that occurred at north coast off Kitakyushu and NW/W/SW/E coast off Tsushima Island on June to September period whose lengths were detected between 6-28 km and wavelength between 120m-1.28km. The directions of internal wave propagation were varied between NW-SW at eastern channel and N-SW at western channel of Tsushima Strait.
机译:在本文中,小波分析已用于1993-2004年期间日本西南对马海峡的ERS SAR和ASTER图像数据中的内部波检测。各种小波变换对Haar小波,Symlet小波,Biorthogonal小波,Coif小波和Daubechies小波在水平,对角和垂直细节上与不同级别的合成图像进行了比较测试,并近似研究了图像的内部波特性。 在2-5级图像变换的水平和垂直细节系数上,内部波特征被检测为图像中的拉长图案,其小波系数(> 36)比海面(<10)高。分解图显示 小波变换分解内部波特征的趋势倾向于遵循小波函数。这可能会减小前导波的高度。使用更高的分辩率可以形成更平滑的内部波形结果 级别5和更高消失矩数量的图像,例如Daubechies wavelet-db5,Symlet wavelet-sym5和Discrete Meyer小波。提出了具有尺度函数和FIR滤波器的正交基紧支持的小波函数,例如离散Meyer函数,以实现特征的平滑性,节省空间的编码并避免图像中的脱皮。 到目前为止,对6月至9月在北九州岛北海岸和对马岛西北部NW / W / SW / E海岸发生的内波数据进行了很好的探测,探测到的长度在6-28 km之间,波长在120m-1.28km。对马海峡东部海峡西南风和西海峡西部海浪的内部波传播方向有所不同。

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