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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Mid-depth internal wave energy off the Iberian Peninsula estimated from seismic reflection data
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Mid-depth internal wave energy off the Iberian Peninsula estimated from seismic reflection data

机译:根据地震反射数据估算的伊比利亚半岛中深度内波能量

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Energy levels of internal waves are estimated from seismic reflection data. Three legacy seismic sections from 1993 and 1997 obtained off the Iberian Peninsula have been analyzed for acoustic reflections within the water column. The reflections are aligned continuously for up to several kilometers over large parts of the sections and in the depth interval from 200 to 2000 m. Depth variations of these reflections are thought to be caused by the background internal wave field. From the variations we derive horizontal wave number spectra of normalized internal wave displacement. The general slope of the power density spectra is remarkably consistent for all sections and agrees well with model spectra for internal waves. Significant differences within the sections can be found when sufficiently large subsections are averaged. The spatial variation of the energy level indicates increasing internal wave activity with shallower water depths as well as near a subsurface eddy.
机译:内部波的能级是根据地震反射数据估算的。对伊比利亚半岛1993年和1997年的三个遗留地震剖面进行了分析,以分析水柱内的声反射。反射在截面的大部分区域以200至2000 m的深度间隔连续排列长达数公里。这些反射的深度变化被认为是由背景内部波场引起的。从这些变化中,我们得出归一化内部波位移的水平波数谱。功率密度谱的总体斜率在所有截面上都非常一致,并且与内部波的模型谱非常吻合。当平均足够大的子部分时,可以发现这些部分之间存在显着差异。能级的空间变化表明随着浅水深度以及地下涡流的增加,内波活动增加。

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