Time-Domain Full Waveform Inversion Using the Gradient Preconditioning Based on Transmitted Wave Energy

The gradient preconditioning approach based on seismic wave energy can effectively avoid the huge memory consumption of the gradient preconditioning algorithms based on the Hessian matrix. However, the accuracy of this approach is prone to be influenced by the energy of reflected waves. To tackle this problem, the paper proposes a new gradient preconditioning method based on the energy of transmitted waves. The approach scales the gradient through a precondition factor, which is calculated by the ‘approximate transmission wavefield' simulation based on the nonreflecting acoustic wave equation. The method requires no computing nor storing of the Hessian matrix and its inverse matrix. Furthermore, the proposed method can effectively eliminate the effects of geometric spreading and disproportionality in the gradient illumination. The results of model experiments show that the time-domain full waveform inversion(FWI) using the gradient preconditioning based on transmitted wave energy can achieve higher inversion accuracy for deep high-velocity bodies and their underlying strata in comparison with the one using the gradient preconditioning based on seismic wave energy. The field marine seismic data test shows that our proposed method is also highly applicable to the FWI of field marine seismic data.     

中国人海经济系统环境适应性演化及预警

基于敏感性-稳定性-响应3维要素构建指标体系,运用熵值法和ARIMA-BP组合预测模型研究中国人海经济系统环境适应性的演化及预警。结果表明：① 2001~2016年中国人海经济系统环境适应性呈稳定上升态势,总体集中于中警状态,期间经历了“人海环境系统比较优势阶段→耦合协调阶段→人海经济系统比较优势阶段”的双螺旋适应过程,预计2017~2020年再次进入相互契合的轻警状态;② 16 a间中国人海经济系统环境适应性波动存在上升期短-衰退期长现象,预计未来4 a人海经济系统环境适应性在经济下行和生态约束背景下的速率不容乐观;③ 权衡人海经济系统和人海环境系统的关系,追求总体效益最大化,延长适应性周期波动中扩张期活动,差别化和灵活性的适应行为是未来主要排警对策。     

褐菖鲉仔、稚鱼消化系统发育的组织学观察

为探究卵胎生鱼类褐菖鲉(Sebastiscus marmoratus)的仔、稚鱼消化系统组织学特点, 采用常规组织切片技术, 并用HE染色和组织化学染色, 比较分析了产出后0~50d的褐菖鲉仔、稚鱼消化系统发育的组织学变化。结果显示: 褐菖鲉初产仔鱼已分化出口咽腔, 并具有初始的食道、胃、肠、肝脏和胰脏; 2日仔鱼肛门与外界相通, 食道扩大, 开始摄食, 进入混合性营养期; 3~4日仔鱼幽门盲囊出现, 食道内壁出现黏膜皱褶5~6个, 胃黏膜皱褶5个, 肝细胞团区域扩大; 5~6日仔鱼卵黄囊和油球耗尽, 进入外源性营养期, 食道黏膜上皮出现杯状细胞, 肠道弯曲, 可区分前中肠和后肠两部分; 10~14日仔鱼食道环肌层明显, 黏膜皱褶增加到7~12个, 胃壁四层结构基本形成, 肠道黏膜皱褶加深, 纹状缘清晰可见, 肝细胞分裂迅速, 数量显著增加, 体积增大, 出现肝血窦和胰岛; 28~30日稚鱼出现胃腺和胃小凹, 已具功能性胃, 标志着稚鱼期的开始, 此时胰岛细胞数量和酶原颗粒增多, 消化能力显著提高; 47~50日稚鱼已基本具有成鱼胃的特征, 肠道纹状缘发达, 肝细胞呈多边形, 细胞内含大量脂肪颗粒, 消化系统从结构和功能上已趋于完善。由此可见, 褐菖鲉仔鱼和稚鱼消化系统的发育具有卵胎生鱼类发育较早的特点, 与其消化功能的完善密切相关。     

浅析WAAS完好性算法

广域增强系统完好性是度量系统时空可用性的关键指标,它关系到用户所获得的改正信息是否真实可靠。在阐述广域增强系统完好性定义的基础上,对完好性算法流程、思路进行了分析。     

洪灾风险评价与区划研究进展

洪灾风险评价是洪灾风险管理的首要步骤。洪灾风险区划是在洪灾风险评价基础上的宏 观分区, 有助于更清晰的把握洪灾风险的空间格局与内在规律。文章首先对洪灾风险相关概念进 行了阐述, 试图达到理清和规范的目的。然后对洪灾风险评价常用方法和洪灾风险区划研究进行 了评述。目前主要的洪灾风险评价方法有地貌学方法、水文水力学模型与系统仿真模拟方法、基 于历史灾情数据的方法、基于水灾史料和古洪水调查的方法、遥感与GIS 方法、基于洪灾形成机 制的系统分析方法等。最后对洪灾风险评价与洪灾风险区划研究进行了小结, 并指出了未来在洪 灾风险评价与区划的数据基础、洪灾风险评价的时空尺度、洪灾风险区划的理论与方法、洪灾风 险评价与区划的技术手段等方面的可能发展前景。     

Seasonal variability of intrusion of the Kuroshio water across the continental shelf northeast of Taiwan

The currents over the East China Sea continental slope northeast of Taiwan were monitored from mid-July to early December, 1992 and again from late March to early August, 1993, covering the two transition periods of monsoon seasons. In 1992, we found massive Kuroshio intrusion (onshore velocity reaching 25 cm/s or more) occurred at mid-October, a lag of one month after the wind pattern changed from southerly to northeasterly. By comparing the surface meteorological with observed cross-slope velocity, we suggest that cooling rather than direct wind forcing, i.e., mid-October cold air outbreaks associated with the Siberia highs moving across the East China Sea, may be the major cause for triggering the observed winter intrusion event. The intrusion continued until the end of the 1992 data in early December and again in late March and early April of 1993 when the data became available. In mid-April, 1993, the intrusion suddenly halted when the lows replaced the highs and the wind reversed with warm air from south. In addition, we found that short-period intrusions appeared in August and early September, 1992 and in late July, 1993. All of these summer intrusions coincide with the occurrence of typhoon passages over or further offshore of the area northeast of Taiwan.     

Dynamics of subtidal flow in the Taiwan Strait

Two current meter moorings were deployed in the Taiwan Strait from 3 April to 5 May 1983. The data indicate that the subtidal flow in this rather wide strait can be separated into two parts: the mean flow and wind-driven flow, which make about equal contributions to the overall flow. The mean flow is probably originates from branching of the Kuroshio through Bashi Channel. The magnitude of the current is nearly 30 cm sec^–1 flowing northward, and the corresponding along-strait sea surface slope is on the order of 10^–7. The residual flow is a local wind-driven flow, and reaches a frictionally balanced state in about 4 hr. Assuming a linear drag law for the bottom stress, a hindcast scheme is constructed and the results compare well with the observations.     

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基于激光反射率的点云与图像自动融合

提出一个基于激光反射率的点云图像自动融合算法,数字图像与点云反射率图像特征点匹配,得到数字图像特征点像点坐标和相应物点物方空间坐标对,采用直接线性变换算法(DLT)建立点云数据反投影至二维图像点的投影模型,实现点云图像自动融合,得到目标表面的全面信息,包括物体表面三维坐标和纹理信息。自动地实现点云图像融合,无需人工参与,提高效率和准确率,同时结合实验验证该算法的可行性。