We assembled approximately 328 seismic records. The data set was from 4 digitally recording long-period and broadband stations of CDSN. We carried out the inversion based on the partitioned waveform inversion (PWI). I...We assembled approximately 328 seismic records. The data set was from 4 digitally recording long-period and broadband stations of CDSN. We carried out the inversion based on the partitioned waveform inversion (PWI). It partitions the large-scale optimization problem into a number of independent small-scale problems. We adopted surface waveform inversion with an equal block (2((2() discretization in order to acquire the images of shear velocity structure at different depths (from surface to 430 km) in the crust and upper-mantle. The resolution of all these anomalies has been established with (check-board( resolution tests. These results show significant difference in velocity, lithosphere and asthenosphere structure between South China Sea and its adjacent regions.展开更多
Based on intensity data in Shanghai and its adjacent region, the intensity attenuation relation is determined. Selecting the western United States as a reference area where there are rich strong ground motion records ...Based on intensity data in Shanghai and its adjacent region, the intensity attenuation relation is determined. Selecting the western United States as a reference area where there are rich strong ground motion records and intensity data, and by determining ground motion attenuation relation in an area lacking in strong ground motion data, we obtain the ground motion attenuation relation in Shanghai and its adjacent region.展开更多
In this paper,climatic features of sea temperature of western Pacific warm pool and the relationship with sea surface temperature (SST) of its adjacent regions are analyzed based on the observed sea temperature on ver...In this paper,climatic features of sea temperature of western Pacific warm pool and the relationship with sea surface temperature (SST) of its adjacent regions are analyzed based on the observed sea temperature on vertical cross section along 137°E in western Pacific,the monthly mean SST of Xisha Station in South China Sea and the global monthly mean SST with resolution of 1°×1°(U.K./GISST2.2).The results indicate that (1) in a sense of correlation.SST of western Pacific warm pool can represent its sea subsurface temperature from surface to 200 m-depth level in winter,and it can only represent sea temperature from surface to 70 m depth in summer.The sea subsurface temperature anomaly of warm pool may be more suitable for representing thermal regime of western Pacific warm pool.The sea subsurface temperature of warm pool has a characteristic of quasi-biennial oscillation.(2)Warm pool and Kuroshio current are subject to different ocean current systems (3)Furthermore,the relationship between SST of Xisha Station and SST of warm pool has a characteristic of negative correlation in winter and positive correlation in summer,and a better lag negative correlation of SST of Xisha Station with sea subsurface temperature of warm pool exists.(4)Additionally,oscillation structure of sea temperature like “a seesaw” exists in between warm pool and Regions Nino3 and Nino4.January (June) maximum (minimum) sea subsurface temperature anomaly of warm pool may serve as a strong signal that indicates maturity phase (development phase) of La Nina (El Nino) event,it also acts as a strong signal which reveals variations of SST of Regions Nino3 and Nino4.展开更多
采用蒙特卡罗方法建立地海交界分区域复合粗糙面模型,陆地区域采用高斯谱模拟,近海海面区域采用基于变浅系数的北海海浪工程(joint North Sea wave project,JONSWAP)谱模拟;提出了基于分形理论的边界赋形方法,并运用多种反正切权函数处...采用蒙特卡罗方法建立地海交界分区域复合粗糙面模型,陆地区域采用高斯谱模拟,近海海面区域采用基于变浅系数的北海海浪工程(joint North Sea wave project,JONSWAP)谱模拟;提出了基于分形理论的边界赋形方法,并运用多种反正切权函数处理实现了线型、月牙型、峡谷型和分形型边界的地海交界环境;基于矩量法和基尔霍夫近似的混合算法研究了地海交界环境与其上方双目标的复合电磁散射特性,对比了双目标分别位于两种典型环境和地海交界环境上方时的复合散射系数曲线,研究了复合散射系数随入射角、陆地区域参数、海面参数、边界形状、双目标参数及双目标类型的变化情况,并做了详细分析与讨论。结果表明该混合算法的高效性和准确性,数值仿真结果对地海交界环境上方目标的探测、遥感及成像具有借鉴意义。展开更多
基金State Natural Scientific Foundation (49734150) and National High Performance Computation Foundation.
文摘We assembled approximately 328 seismic records. The data set was from 4 digitally recording long-period and broadband stations of CDSN. We carried out the inversion based on the partitioned waveform inversion (PWI). It partitions the large-scale optimization problem into a number of independent small-scale problems. We adopted surface waveform inversion with an equal block (2((2() discretization in order to acquire the images of shear velocity structure at different depths (from surface to 430 km) in the crust and upper-mantle. The resolution of all these anomalies has been established with (check-board( resolution tests. These results show significant difference in velocity, lithosphere and asthenosphere structure between South China Sea and its adjacent regions.
文摘Based on intensity data in Shanghai and its adjacent region, the intensity attenuation relation is determined. Selecting the western United States as a reference area where there are rich strong ground motion records and intensity data, and by determining ground motion attenuation relation in an area lacking in strong ground motion data, we obtain the ground motion attenuation relation in Shanghai and its adjacent region.
基金Supported by National Natural Science Foundation of China,the Grant number of 49775270 and 49775267.the Chinese Academy of Sciences Project(KZ951-A1-402)
文摘In this paper,climatic features of sea temperature of western Pacific warm pool and the relationship with sea surface temperature (SST) of its adjacent regions are analyzed based on the observed sea temperature on vertical cross section along 137°E in western Pacific,the monthly mean SST of Xisha Station in South China Sea and the global monthly mean SST with resolution of 1°×1°(U.K./GISST2.2).The results indicate that (1) in a sense of correlation.SST of western Pacific warm pool can represent its sea subsurface temperature from surface to 200 m-depth level in winter,and it can only represent sea temperature from surface to 70 m depth in summer.The sea subsurface temperature anomaly of warm pool may be more suitable for representing thermal regime of western Pacific warm pool.The sea subsurface temperature of warm pool has a characteristic of quasi-biennial oscillation.(2)Warm pool and Kuroshio current are subject to different ocean current systems (3)Furthermore,the relationship between SST of Xisha Station and SST of warm pool has a characteristic of negative correlation in winter and positive correlation in summer,and a better lag negative correlation of SST of Xisha Station with sea subsurface temperature of warm pool exists.(4)Additionally,oscillation structure of sea temperature like “a seesaw” exists in between warm pool and Regions Nino3 and Nino4.January (June) maximum (minimum) sea subsurface temperature anomaly of warm pool may serve as a strong signal that indicates maturity phase (development phase) of La Nina (El Nino) event,it also acts as a strong signal which reveals variations of SST of Regions Nino3 and Nino4.
文摘采用蒙特卡罗方法建立地海交界分区域复合粗糙面模型,陆地区域采用高斯谱模拟,近海海面区域采用基于变浅系数的北海海浪工程(joint North Sea wave project,JONSWAP)谱模拟;提出了基于分形理论的边界赋形方法,并运用多种反正切权函数处理实现了线型、月牙型、峡谷型和分形型边界的地海交界环境;基于矩量法和基尔霍夫近似的混合算法研究了地海交界环境与其上方双目标的复合电磁散射特性,对比了双目标分别位于两种典型环境和地海交界环境上方时的复合散射系数曲线,研究了复合散射系数随入射角、陆地区域参数、海面参数、边界形状、双目标参数及双目标类型的变化情况,并做了详细分析与讨论。结果表明该混合算法的高效性和准确性,数值仿真结果对地海交界环境上方目标的探测、遥感及成像具有借鉴意义。
