The Euler angle estimation is a calibration method for vector data measured by the magnetometer on a satellite.It is used to find the relative rotation between the coordinate system of the magnetometer and the satelli...The Euler angle estimation is a calibration method for vector data measured by the magnetometer on a satellite.It is used to find the relative rotation between the coordinate system of the magnetometer and the satellite(usually determined by Star Imagers).Before launch of the low-orbit,low-inclination Macao Science Satellite-1(known as MSS-1),we simulated the estimation of Euler angles by using the magnetic measurements of the in-orbit Swarm and China Seismo-Electromagnetic Satellite(noted as CSES),with various data combinations.In this study,11 data sets were designed to analyze the estimation results for the MSS-1 orbit by using a joint estimation method of the geomagnetic field model parameters and Euler angles.For the model results,we found that all the spatial power spectral lines showed behavior consistent with that of the CHAOS-7.8 model at low degrees(corresponding to large-scale magnetic signals).The spectra of models without global data coverage deviated much more(by a maximum of~10^(4) nT^(2))from those of the CHAOS-7.8 model at higher degrees.For models with global data coverage and with various data combinations,the spectral lines were distributed similarly.Moreover,the models with accordant power spectral distributions demonstrated different Euler angle estimations.As more vector data at higher latitudes were included,the estimated Euler angles varied monotonically in all three directions.The models with vector data in the same latitude range showed similar Euler angle results,regardless of whether the poleward scalar data were included.The largest value difference was found between the models using vector data within±40°latitudes and those using vector data within±60°latitudes,which reached to~28″.Therefore,we concluded that the inversion of the spherical harmonic Gauss coefficients in our tests was mainly affected by the spatial coverage range of the data,whereas the estimation of Euler angles largely depended on the latitude range where the vector data could be obtained.These results can be展开更多
对白令海北部陆坡B5-4孔进行了古地磁和岩石磁学研究,尝试获得该岩芯的地磁场相对强度和方向变化信息.结果表明：（1）除0～0.44m沉积物的磁性矿物粒度比其余沉积物细以外,岩芯的磁学性质总体均一,其记录的地磁场相对强度可以与北大西洋...对白令海北部陆坡B5-4孔进行了古地磁和岩石磁学研究,尝试获得该岩芯的地磁场相对强度和方向变化信息.结果表明：（1）除0～0.44m沉积物的磁性矿物粒度比其余沉积物细以外,岩芯的磁学性质总体均一,其记录的地磁场相对强度可以与北大西洋ODP983孔相应记录进行高度对比.（2）根据B5-4孔与ODP983孔地磁场相对强度记录对比结果,并结合该孔4.54～4.56 m处有孔虫AMS14C测年结果,可以确定3个深度-年龄对比点,并据此初步建立了B5-4孔的年龄模型.（3）B5-4孔磁偏角和磁倾角记录与贝加尔湖、北美、欧洲全新世以来的记录和当地地磁场球谐模型结果一致,其对比点丰富了强度对比点年龄模型,揭示了14 cal ka B.P.以来近线性的沉积模式.（4）根据与中国东部陆架两个钻孔的磁倾角对比,我们推测B5-4孔9～14 ka之间两段浅化的磁倾角可能是哥德堡极性事件的记录,但是受到早期成岩或者沉积物平滑效应的影响.以上结果足以证明,地磁场相对强度和方向变化可以从适宜的白令海沉积物中获得,它可以为确定该海区沉积物年龄提供相关辅助信息,有助于解决北极、亚北极古环境和古海洋研究中由于有孔虫等钙质生物壳体缺乏导致的年龄信息匮乏问题.展开更多
基金funded by the Macao Foundation,the pre-research project of Civil Aerospace Technologies(Nos.D020308 and D020303)funded by the China National Space Administration,Macao Science and Technology Development Fund(FDCT+1 种基金No.0001/2019/A1)the opening fund of the State Key Laboratory of Lunar and Planetary Sciences(Macao University of Science and Technology,Macao FDCT No.119/2017/A3)。
文摘The Euler angle estimation is a calibration method for vector data measured by the magnetometer on a satellite.It is used to find the relative rotation between the coordinate system of the magnetometer and the satellite(usually determined by Star Imagers).Before launch of the low-orbit,low-inclination Macao Science Satellite-1(known as MSS-1),we simulated the estimation of Euler angles by using the magnetic measurements of the in-orbit Swarm and China Seismo-Electromagnetic Satellite(noted as CSES),with various data combinations.In this study,11 data sets were designed to analyze the estimation results for the MSS-1 orbit by using a joint estimation method of the geomagnetic field model parameters and Euler angles.For the model results,we found that all the spatial power spectral lines showed behavior consistent with that of the CHAOS-7.8 model at low degrees(corresponding to large-scale magnetic signals).The spectra of models without global data coverage deviated much more(by a maximum of~10^(4) nT^(2))from those of the CHAOS-7.8 model at higher degrees.For models with global data coverage and with various data combinations,the spectral lines were distributed similarly.Moreover,the models with accordant power spectral distributions demonstrated different Euler angle estimations.As more vector data at higher latitudes were included,the estimated Euler angles varied monotonically in all three directions.The models with vector data in the same latitude range showed similar Euler angle results,regardless of whether the poleward scalar data were included.The largest value difference was found between the models using vector data within±40°latitudes and those using vector data within±60°latitudes,which reached to~28″.Therefore,we concluded that the inversion of the spherical harmonic Gauss coefficients in our tests was mainly affected by the spatial coverage range of the data,whereas the estimation of Euler angles largely depended on the latitude range where the vector data could be obtained.These results can be
文摘对白令海北部陆坡B5-4孔进行了古地磁和岩石磁学研究,尝试获得该岩芯的地磁场相对强度和方向变化信息.结果表明：（1）除0～0.44m沉积物的磁性矿物粒度比其余沉积物细以外,岩芯的磁学性质总体均一,其记录的地磁场相对强度可以与北大西洋ODP983孔相应记录进行高度对比.（2）根据B5-4孔与ODP983孔地磁场相对强度记录对比结果,并结合该孔4.54～4.56 m处有孔虫AMS14C测年结果,可以确定3个深度-年龄对比点,并据此初步建立了B5-4孔的年龄模型.（3）B5-4孔磁偏角和磁倾角记录与贝加尔湖、北美、欧洲全新世以来的记录和当地地磁场球谐模型结果一致,其对比点丰富了强度对比点年龄模型,揭示了14 cal ka B.P.以来近线性的沉积模式.（4）根据与中国东部陆架两个钻孔的磁倾角对比,我们推测B5-4孔9～14 ka之间两段浅化的磁倾角可能是哥德堡极性事件的记录,但是受到早期成岩或者沉积物平滑效应的影响.以上结果足以证明,地磁场相对强度和方向变化可以从适宜的白令海沉积物中获得,它可以为确定该海区沉积物年龄提供相关辅助信息,有助于解决北极、亚北极古环境和古海洋研究中由于有孔虫等钙质生物壳体缺乏导致的年龄信息匮乏问题.
