Shallow water body data processing based on the seismic oceanography     

LIU Huaishan  HU Yi  YIN Yanxin  WANG Linfei  TONG Siyou  MA Hai 《中国海洋大学学报(英文版)》2013,12(3):319-326

Physical properties of sea water,such as salinity,temperature,density and acoustic velocity,could be demarcated through degradation of energy caused by water absorption,attenuation and other factors.To overcome the challenging difficulties in the quick monitoring of these physical properties,we have explored the high resolution marine seismic survey to instantly characterize them.Based on the unique wavefield propagating in the sea water,we have developed a new approach to suppress the noise caused by the shallow sea water disturbance and obtain useful information for estimating the sea water structure.This approach improves seismic data with high signal-to-noise ratio and resolution.The seismic reflection imaging can map the sea water structure acoustically.Combined with the knowledge of local water body structure profile over years,the instant model for predicting the sea water properties could be built using the seismic data acquired from the specially designed high precision marine seismic acquisition.This model can also be updated with instant observation and the complete data processing system.The present study has the potential value to many applications,such as 3D sea water monitoring,engineering evaluation,geological disaster assessment and environmental assessment.  相似文献   

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傅露  褚永海 《大地测量与地球动力学》2013,33(2):110-113

???DNSC08-GRA????е????????????????????????????????Stokes??????????????????????????????????????????????Stokes????????-??????????????????3.4 cm???????????????????????????????GPS/????????м??????????????????????1.17 m???????????????С?7 cm??  相似文献   

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郭爱智  王勇  刘根友  郑晖  张茂顺 《大地测量与地球动力学》2013,33(5):34-38

?????????????λ??????????????????????????????????t??????????????????????????????????????????????????λ?????GPS????????????????????????????mm/s?????????????1 cm/s??  相似文献   

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王甫红龚学文  徐其超张 蔚 《大地测量与地球动力学》2013,33(6):107-111

????JPL DE?????????洢??????????????????????????????????DE??????????????????????????20???DE406?????????????369 kb????????1/6????GPS??????????ü???DE????????????????????飬?????????60?????????????????????3 m???ü??????????????????????????????????????????????С?????????洢??????????????????????Ч???  相似文献   

2003年青海德令哈6.7级地震序列的震源机制解及其构造含义          下载免费PDF全文

孙长虹  许丰  杨玉波  钱荣毅  孟小红 《地球物理学报》2012,55(10):3338-3346

利用8个流动数字地震台和国家数字地震台站的地震波形记录,测量了2003年4月17日青海德令哈6.7级地震及其主要余震的直达P波、SV波、SH波的初动方向和振幅比,应用Snoke(2003)的测定震源机制解的格点尝试法,测定出德令哈地震序列的48个2.4级以上地震的震源机制解.搜集分析了美国哈佛大学测定的德令哈6.7级主震和2004年二期地震活动中的7个地震的震源机制解.基于余震空间分布特征和对震源机制解特征的分析,讨论了德令哈地震序列的可能断层活动方式和地震的构造含义.结果表明,主震和大部分余震都是沿NWW-SEE走向的逆断层错动,北边的上盘可能沿低角度向北倾的断层面向南仰冲;个别正断层余震可能是震源区挤压变形弧顶区附近发生的局部张性破裂;在二期地震活动中,逆断层和走滑断层都有,走滑断层地震主要发生在震源区东侧.德令哈地震活动是青藏高原东北缘NWW-SEE向延伸的挤压带继续处于隆升活动中的表现,这一继承性新构造运动是德令哈地震序列的可能发震原因.  相似文献   

Improved estimators of correlation and R2 for skewed hydrologic data     

《水文科学杂志》2012,57(1):87-101

ABSTRACT

The coefficient of determination R² and Pearson correlation coefficient ρ = R are standard metrics in hydrology for the evaluation of the goodness of fit between model simulations and observations, and as measures of the degree of dependence of one variable upon another. We show that the standard product moment estimator of ρ, termed r, while well-behaved for bivariate normal data, is upward biased and highly variable for bivariate non-normal data. We introduce three alternative estimators of ρ which are nearly unbiased and exhibit much less variability than r for non-normal data. We also document remarkable upward bias and tremendous increases in variability associated with r using both synthetic data and daily streamflow simulations from 905 calibrated rainfall–runoff models. We show that estimators of ρ = R accounting for skewness are needed for daily streamflow series because they exhibit high variability and skewness compared to, for example, monthly/annual series, where r should perform well.  相似文献   

震后城市地震动场快速评估方法——以福州盆地为例     

丁海平  卜超鹏  杨朝辉 《地震工程与工程振动》2012,32(1):11-15

震后灾情的快速获取是灾后应急的基础,传统的方法是根据现场调查结果决定应急方案。受灾程度的分布常以烈度分布图描述,而烈度又与加速度峰值密切相关。本文提出了一种震后地震动场分布快速评估的方法。该方法将主要依据灾区基岩台站的实时强震记录(无强震记录也行)和该地区的加速度衰减关系,再结合该地区各类场地的地震动放大因子,则可快速估计该地区地震动场分布,从而确定灾情,为政府的应急决策提供依据。  相似文献   

基于MYSQL数据库的地震震相走时系统编制与应用     

隆爱军  夏仕安  王燚坤  陈海博 《地震地磁观测与研究》2012,33(1):105-107

介绍在网络环境下地震震相走时表系统编制的相关技术和流程,阐述该系统特点及使用方法.该震相走时系统在安徽省地震台站应用后,速报时间缩短,地震震相分析精度提高,收到预期效果.  相似文献   

基于星载GPS的HY-2卫星高精度精密定轨模拟研究(英文)   总被引：2，自引：0，他引：2  

郭金运  秦建  孔巧丽  李国伟 《应用地球物理》2012,9(1):95-107

HY-2卫星是我国第一颗测高卫星,其径向定轨精度要求厘米量级,搭载了星载GPS接收机。目前HY-2还处于测试阶段,没有公布观测数据。为了确定基于星载GPS的HY-2精密定轨流程及其定轨精度,本文模拟了HY-2卫星星载GPS观测数据,结果表明HY-2星载GPS天线每个历元至少观测7颗GPS卫星。给出了基于星载GPS的精密定轨流程,分别采用简化动力学方法和动态几何法进行了精密定轨实验。对于相位1mm和3mm随机误差的相位观测数据,简化动力学法和动态几何法定轨都能够实现厘米量级的径向精密定轨,几何法定轨精度略低于简化动力定轨。地球重力场模型是影响HY-2卫星精密定轨的重要因素,本文对不同阶次的重力场模型EIGEN2、EGM96、TEG4和GEMT3进行了简化动力学定轨实验,高于50阶次的重力场模型都能够实现厘米级径向精密定轨,主要原因在于大量的高精度星载GPS观测数据和重力场模型精度的提高。  相似文献   

地震计灵敏度的对比测量法   总被引：2，自引：0，他引：2  

林湛  薛兵  朱小毅  陈阳  李江  彭朝勇  刘洋君 《地震》2013,33(1):22-28

本文提出一种地震计灵敏度的对比测量法, 该方法将被测地震计和一台校准过的地震计比邻、 平行摆放, 共同记录地振动数据, 通过对比分析两台地震计的输出信号, 计算被测地震计的灵敏度。 与振动台测量法相比, 该方法成本低, 与电测法相比, 不需已知地震计的标定常数, 是一种简单易行、 精度高的地震计灵敏度测量方法。  相似文献