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用反射地震方法研究物理海洋—地震海洋学简介
引用本文:宋海斌,董崇志,陈林,宋洋.用反射地震方法研究物理海洋—地震海洋学简介[J].地球物理学进展,2008,23(4):1156-1164.
作者姓名:宋海斌  董崇志  陈林  宋洋
作者单位:1. 中国科学院地质与地球物理研究所地球深部重点实验室,北京,100029
2. 中国科学院地质与地球物理研究所地球深部重点实验室,北京100029;中国科学院研究生院,北京100049
基金项目:国家重点基础研究发展计划(973计划),欧盟资助项目
摘    要:地震海洋学是通过传统反射地震勘探方法研究物理海洋学的一种新方法.相对于传统的接触式温盐深测量方法,该方法具有较高的横向分辨率和能快速对整个海水剖面成像等优点,是一种非常有前途的新方法.本文将详细阐述反射地震方法在探测海洋锋温盐细结构、刻画水团边界、海洋内波、黑潮等方面的研究进展.目前海水层温度差异主要通过叠加剖面的反射轴振幅计算得到,但是叠加剖面并没有做真振幅处理.为了解决计算过程中的误差,最后提出在地震海洋学仲利用真振幅偏移结果可以使计算更加合理的设想.

关 键 词:地震海洋学  海洋锋  温盐细微结构  海洋内波  真振幅偏移
收稿时间:2008-2-10
修稿时间:2008-6-20

Reflection seismic methods for studying physical oceanography: Introduction of seismic oceanography
SONG Hai-bin,DONG Chong-zhi,CHEN Lin,SONG Yang.Reflection seismic methods for studying physical oceanography: Introduction of seismic oceanography[J].Progress in Geophysics,2008,23(4):1156-1164.
Authors:SONG Hai-bin  DONG Chong-zhi  CHEN Lin  SONG Yang
Abstract:Seismic oceanography is a promising new tool for studies of physical oceanography which uses conventional low frequency marine seismic reflection techniques. Compared to the traditional methods of probing the ocean, they offer several advantages, such as enhanced lateral resolution, the ability to simultaneously image large sections of the ocean, and opportunities for three-dimensional and time-lapse imaging. The paper introduces the research progress on several important oceanic phenomena, including measuring thermohaline fine structure, imaging water mass boundaries, internal wave and the Kuroshio Current. Recently the seismic stacked sections are not considered as true amplitude processed, so the temperature contrasts, which are calculated by the amplitudes of post-stack sections, are not accurate. Finally, we present an idea of using new true amplitude migration method which can make the result more sense in seismic oceanography research.
Keywords:seismic oceanography  oceanographic front  thermohaline fine structure  internal wave  true amplitude migration
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