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Detecting overlapping gravity waves using the S-Transform

机译:使用S变换检测重叠的重力波

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We discuss an adaptation to the widely-used Stockwell Transform based method for the detection of gravity waves to allow the detection of multiple overlapping waves. This adjusted method is applied to data from the High Resolution Dynamics Limb Sounder for the period of May 2006 and is found to change the measured distribution of gravity wave momentum flux on a global scale. An overall 68% increase in measured momentum flux is observed for the 20-30km altitude range, with significant regional variability. The largest absolute increase is over India, the Southern Ocean, and the Antarctic Peninsula, regions previously known to exhibit high levels of momentum flux. A strong relative increase is observed north of the equator, particularly in the tropics; analysis of the wavelength distribution of detected gravity waves shows that the majority of this increase is due to the detection of small vertical- and horizontal-scale waves which were presumably previously masked by higher-amplitude events in the same profile. Key PointsIncluding secondary waves increases measured MF by 68%The geographic distribution is alteredThis is most important in convective regions
机译:我们讨论了一种对广泛使用的基于Stockwell变换的方法的改编,该方法用于检测重力波以允许检测多个重叠波。该调整后的方法应用于高分辨率动力学肢体测深仪2006年5月的数据,发现该方法在全球范围内改变了测得的重力波动量通量分布。在20-30公里的海拔范围内,观测到的动量通量总体增加了68%,区域差异很大。绝对增幅最大的地区是印度,南大洋和南极半岛,这些地区以前已知表现出高水平的动量通量。在赤道以北,特别是在热带地区,观测到相对较大的增加。对检测到的重力波的波长分布的分析表明,这种增加的大部分是由于检测到了小的垂直和水平尺度的波,这些波以前大概被同一幅图中的高振幅事件掩盖了。要点包括次波将测得的MF提高68%地理分布发生变化这在对流地区最重要

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