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利用反射地震数据和XBT数据联合反演海水的温盐分布
引用本文:黄兴辉,宋海斌,Luis M.Hnheiro,拜阳.利用反射地震数据和XBT数据联合反演海水的温盐分布[J].地球物理学报,2011,54(5):1293-1300.
作者姓名:黄兴辉  宋海斌  Luis M.Hnheiro  拜阳
作者单位:1. 中国科学院地质与地球物理研究所,中国科学院油气资源研究重点实验室,北京 100029; 2. 中国科学院研究生院,北京 100049; 3. CESAM and Departamento de Geociências , Universidade de Aveiro, 3800 Aveiro, Portugal
基金项目:国家自然科学基金,国家基础研究发展规划项目,欧盟NEST (New and Emerging Science and Technology)项目
摘    要:利用地震数据反演海水的温盐分布是地震海洋学研究的一个重要方向.本文分析了采集于伊比利亚半岛西南缘海域的GOLR12低频地震数据和同步观测的XBT(eXpendable BathyThermograph)、CTD(Conductivity-Temperature-Depth)资料,将叠后约束波阻抗反演方法应用到海水温度、盐度剖面的计算当中,计算结果显示这种反演方法可以提供水平分辨率为6.25 m的温度和盐度资料,温度的精度约为0.16 ℃,可以为物理海洋学研究提供高横向分辨率的基础数据.

关 键 词:地震海洋学  叠后反演  温盐分布  地中海涡旋  
收稿时间:2010-11-02

Ocean temperature and salinity distributions inverted from combined reflection seismic and XBT data
HUANG Xing-Hui,SONG Hai-Bin,Luis M.Hnheiro,BAI Yang.Ocean temperature and salinity distributions inverted from combined reflection seismic and XBT data[J].Chinese Journal of Geophysics,2011,54(5):1293-1300.
Authors:HUANG Xing-Hui  SONG Hai-Bin  Luis MHnheiro  BAI Yang
Institution:1. Key Laboratory of Petroleum Resources Research, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 3. CESAM and Departamento de Geociências , Universidade de Aveiro, 3800 Aveiro, Portugal
Abstract:Seismic oceanography has been widely used to detect many kinds of oceanographic features as a new oceanographic prospecting method. Inversion for temperature and salinity distributions from seismic data is a very important research field in seismic oceanography. We analyzed low frequency seismic data from one multichannel seismic (MCS) line acquired in the scope of the European GO Project (line GOLR-12) combined with the simultaneously acquired XBT (eXpendable BathyThermograph) and CTD (Conductivity-Temperature-Depth) data, which are located to the southwest of the Iberian Peninsula. We used a post-stack constrained impedance inversion method to derive temperature and salinity distributions of sea water and the result demonstrated that this method can indeed provide reliable temperature and salinity distribution profiles every 6.25m along the seismic line, with the temperature resolution of 0.16℃. This method applied to good quality MCS data can provide high lateral-resolution temperature and salinity profiles for oceanographic research, using only a few oceanographic measurements to constrain the inversion procedure.
Keywords:Seismic oceanography  Post-stack inversion  Temperature and salinity distribution  Meddy
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