海上风、涌浪的存在严重影响高分辨率海洋地震资料的采集质量，而现有的涌浪静校正方法，无论是基于数据自身特征抑或是利用外部信息约束的方法，均有其特定的适用范围与应用局限。基于以上事实，本文提出了一种更具有普适性的基于变分模态分解（VMD）的涌浪静校正技术。首先介绍了VMD的基本原理和涌浪压制的实现步骤，接着对水平层状模型进行了合成数据试算，最后对野外实测资料进行了涌浪压制，并就该方法的可靠性开展了定量计算。结果表明：无论海底地形是简单的平缓起伏还是复杂的崎岖不平，本文VMD方法均能够有效压制涌浪效应引起的同相轴高频抖动、改善能量分散、消除毛刺，使原本混乱模糊的反射层位信息变得清晰、光滑、连续，极大地提高了剖面分辨率及信噪比，有效地提高了后续地层划分及剖面解释精度。

The existence of offshore swell affects the quality of high-resolution marine seismic data collection seriously, while the existing swell static correction methods, neither those based on the characteristics of the data itself nor those using external information constraints, have their certain conditions of application. In view of this prevalent phenomenon, a much more universal swell static correction technique was proposed in this paper. After a simple introduction of basic principle and implementation steps, the swell effect of synthetic data of horizontal layered model was calculated subsequently, and swell suppression was carried out utilizing the surveyed data ultimately, meanwhile the reliability and effectiveness of the proposed method was quantitatively verified. The results show that whether the seafloor is simply gently-undulated or complicatedly rugged, the phenomena of high frequency jitter and energy dispersion in the reflection event caused by the swell effect can be suppressed effectively based on the method we proposed, which make the original confusing and fuzzy reflector much more clear, smooth and continuous and greatly improves the resolution and signal-to-noise ratio of the seismic sections, providing convenience for the subsequent stratigraphic division and seismic section interpretation.