Abstract

Abstract. Seismic oceanography (SO) acquires water column reflections using controlled source seismology and provides high lateral resolution that enables the tracking of the thermohaline structure of the oceans. Most SO studies obtain data using air guns, which can produce acoustic energy below 100 Hz bandwidth, with vertical resolution of approximately 10 m or more. For higher-frequency bands, with vertical resolution ranging from several centimeters to several meters, a smaller, low-cost seismic exploration system may be used, such as a sparker source with central frequencies of 250 Hz or higher. However, the sparker source has a relatively low energy compared to air guns and consequently produces data with a lower signal-to-noise (S∕N) ratio. To attenuate the random noise and extract reliable signal from the low S∕N ratio of sparker SO data without distorting the true shape and amplitude of water column reflections, we applied machine learning. Specifically, we used a denoising convolutional neural network (DnCNN) that efficiently suppresses random noise in a natural image. One of the most important factors of machine learning is the generation of an appropriate training dataset. We generated two different training datasets using synthetic and field data. Models trained with the different training datasets were applied to the test data, and the denoised results were quantitatively compared. To demonstrate the technique, the trained models were applied to an SO sparker seismic dataset acquired in the Ulleung Basin, East Sea (Sea of Japan), and the denoised seismic sections were evaluated. The results show that machine learning can successfully attenuate the random noise in sparker water column seismic reflection data.

Highlights

  • Conventional physical oceanography measurements from cruises are performed by deploying instruments such as a conductivity–temperature–depth (CTD) probe, an expendable conductivity–temperature–depth (XCTD) probe or an expendable bathythermograph (XBT) at observation stations

  • Seismic oceanography (SO) is a method that obtains the water column reflections via seismic exploration and analyzes seismic sections to estimate the oceanographic characteristics of sea water

  • The noise in SO data has been attenuated through simple data processing methods because most of the SO data are obtained with air guns, which generate data with a high S/N ratio

Read more

Summary

Introduction

Conventional physical oceanography measurements from cruises are performed by deploying instruments such as a conductivity–temperature–depth (CTD) probe, an expendable conductivity–temperature–depth (XCTD) probe or an expendable bathythermograph (XBT) at observation stations. Seismic oceanography (SO) is a method that obtains the water column reflections via seismic exploration and analyzes seismic sections to estimate the oceanographic characteristics of sea water. The improvement in vertical resolution is evident when using higher-frequency band sources such as a sparker source; if appropriate methods can effectively suppress the random noise, more useful information can be derived compared to SO data using an air gun source. It is difficult to apply various noise attenuation methods to SO data because analyzing the internal wave and turbulent subranges of the water column requires the horizontal wavenumber spectrum (Klymak and Moum, 2007) of the seismic data, which is liable to be damaged by data processing. The trained models are applied to the Ulleung Basin, East Sea (Sea of Japan) sparker SO data, and the results are compared and evaluated

Review of the DnCNN
Network architecture
Sparker SO data
Training data
Experimental setting
Experiment using training dataset 1
Experiment using training dataset 2
Calculation of the data slope spectrum from the synthetic seismic section
Application to the sparker SO data
Findings
Summary
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call