Multi-Time Scale Analysis of Runoff at the Yangtze Estuary Based on the Morlet Wavelet Transform Method

Runoff series of the Yangtze River presents an intricate variation tendency under the reinforced influence of human activities.The Morlet Wavelet Transform method has been applied to analyze the annual runoff data from 1950 to 2011 at the Yangtze River Estuary.It can clearly reveal the multi-time scales structure,break point,change and distribution of periodic variation in the different time scales of the runoff series.The main conclusions are that：1） Repeated periodic oscillations accompanied by an extremely large fluctuation are presented in the runoff series with an obvious difference between wet and dry years,and the major periods of the time series are about 3,8,16 and 23 years respectively.Among them,the presented maximum periodic oscillation is 23 years scale.2） In the 23-year time scale,the wet periods are 1950-1958,1969-1980 and 1992-2003,and the dry periods are 1959-1968,1981-1991 and 2004-2011.3） It can be predicted from the view of long time scales that the low annual runoff will likely occur in the near future.     

数字区域应用基础设施研究

针对当前数字区域工程建设普遍存在的一些问题,提出“数字区域”应用基础设施的概念,对其研究背景、参考模型和面向信息共享的公共应用服务平台进行了论述。数字区域应用基础设施是在区域网络基础设施和数据基础设施上层的基础设施,它为电子政务、电子商务、数字城市等各种数字区域信息化应用工程提供基础性的应用服务支撑,由专业信息服务机构、管理办法、标准规范、关键技术和公共应用服务平台构成。信息服务机构是数字区域应用基础设施的主体,是有效联系信息需求方和信息拥有方的桥梁;公共应用服务平台是数字区域应用基础设施的核心,为区域信息共享和交换提供了统一的构架和解决方案。其中,元数据管理和目录服务平台为信息的发布和查询提供了“一站式”入口;信息共享与协作服务平台实现了分布式数据库的信息共享和交换;地理空间信息网络服务平台实现了地理空间信息的集中式共享。最后,总结了“数字福建”应用基础设施建设的成果,对“十一五”“数字福建”工程的需求和发展作了展望。     

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?????????????GNSS???????????????????????????λ???????????????????3????????????3??GNSS???????????????GNSS??????????????μ????????????????????????????????????￡??????????????????3????????????????????????????????????????????????????????????????????????????????????????????λ??????????????????????????????з???3.0?????????????????о??д????????????     

1∶50000正射影像数据检查库设计及实现

国家1∶50000基础地理信息数据库更新工程正射影像数据库是1∶50 000数据库更新工程建设的重要组成部分.为保证正射影像数据各项指标符合项目设计要求,保证入库数据的质量,并为今后进一步更新提供依据,设计正射影像数据检查库,并在1∶50 000 DOM更新工程中实施和应用,实现了正射影像数据入库检查的程序化处理和自动质量评判.     

LSQRD及解的分辨分析

较详细地介绍了ＬＳＱＲＤ（Ｌｅａｓｔ Ｓｑｕａｒｅ ＱＲ Ｄｅｃｏｍｐｏｓｉｔｉｏｎ） 反演方法以及“检测版”分辨分析方法,并举实例检验其应用。对于大型稀疏方程组的求解,ＬＳＱＲＤ 是一种内存需求小、计算效率高和抗噪能力较强的算法。“检测版”试验表明,ＬＳＱＲＤ也可以对迭代解进行有效的可靠性估计,以指导对反演结果的利用。     

GML分布式广义空间数据引擎的研究

在解析GML规范与空间数据引擎前沿研究成果的基础上,提出了一种语义对象模式表达的分布式广义空间数据引擎(SDE)模型。在通用大型数据库平台与通信机制支持下,用语义对象模式的GIS语言构建了一个全新的分布式广义SDE模型。对模型开发成果的应用与今后努力的方向作了简要的介绍。     

Numerical study on inter-tidal transports in coastal seas

Inter-tidal(subtidal) transport processes in coastal sea depend on the residual motion, turbulent dispersion and relevant sources/sinks. In Feng et al.(2008), an updated Lagrangian inter-tidal transport equation, as well as new concept of Lagrangian in- ter-tidal concentration(LIC), has been proposed for a general nonlinear shallow water system. In the present study, the LIC is nu- merically applied for the first time to passive tracers in idealized settings and salinity in the Bohai Sea, China. Circulation and tracer motion in the three idealized model seas with different topography or coastline, termed as ‘flat-bottom', ‘stairs' and ‘cape' case, re- spectively, are simulated. The dependence of the LIC on initial tidal phase suggests that the nonlinearities in the stairs and cape cases are stronger than that in the flat-bottom case. Therefore, the ‘flat-bottom' case still meets the convectively weakly nonlinear condi- tion. For the Bohai Sea, the simulation results show that most parts of it still meet the weakly nonlinear condition. However, the de- pendence of the LIS(Lagrangian inter-tidal salinity) on initial tidal phase is significant around the southern headland of the Liaodong Peninsula and near the mouth of the Yellow River. The nonlinearity in the former region is mainly related to the complicated coast- lines, and that in the latter region is due to the presence of the estuarine salinity front.     

Submarine landslide identified in DLW3102 core of the northern continental slope,South China Sea

In this paper, we take DLW3101 core obtained at the top of the canyon(no landslide area) and DLW3102 core obtained at the bottom of the canyon(landslide area) on the northern continental slope of the South China Sea as research objects. The chronostratigraphic framework of the DLW3101 core and elemental strata of the DLW3101 core and the DLW3102 core since MIS5 are established by analyzing oxygen isotope, calcium carbonate content, and X-Ray Fluorescence(XRF) scanning elements. On the basis of the information obtained by analyzing the sedimentary structure and chemical elements in the landslide deposition, we found that the DLW3102 core shows four layers of submarine landslides, and each landslide layer is characterized by high Si, K, Ti, and Fe contents, thereby indicating terrigenous clastic sources. L1(2.15–2.44 m) occurred in MIS2, which is a slump sedimentary layer with a small sliding distance and scale. L2(15.48–16.00 m) occurred in MIS5 and is a debris flow-deposited layer with a scale and sliding distance that are greater than those of L1. L3(19.00–20.90 m) occurred in MIS5; its upper part(19.00–20.00 m) is a debris flow-deposited layer, and its lower part(20.00–20.90 m) is a sliding deposition layer. The landslide scale of L3 is large. L4(22.93–24.27 m) occurred in MIS5; its upper part(22.93–23.50 m) is a turbid sedimentary layer, and its lower part(23.50–24.27m) is a slump sedimentary layer. The landslide scale of L4 is large.     

局部最优形态参数的RBF分块地形插值方法与实验

径向基函数（Radial Basis Function,RBF）是一种不需对数据做任何假设,能准确逼近任意维度数据的空间插值方法。其特别适合于复杂地形的数字高程模型（Digital Elevation Model,DEM）插值重建,但随着已知点数量的增加会导致插值模型求解困难或缓慢。针对这个问题,本文基于二叉树自适应递归分块原理,采用局部最优形态参数的RBF分块插值方法进行DEM插值重建。首先,设定子区域最小点数阈值和相邻子区域的重叠率,自顶向下,对研究区域进行递归分块,构建区域分块二叉树,对二叉树叶子节点区域,采用逐点交叉验证（Leave One Out Cross Validation,LOOCV）方法求解其最优形态参数,建立局部RBF最优插值模型;然后,根据单元分解原理,采用加权平均方法对相应叶子节点区域内的待插值点高程进行加权求和,自底向上递归求解,得到待插值点最终高程值。以云南某地区DEM进行插值实验表明,采用本文方法进行DEM插值重建,稳定性较好,插值精度高。     

陕西镇巴火焰溪法门阶牙形刺研究

陕西镇巴火焰溪剖面位于大巴山西段，临近川陕交界、交通便利。那里晚泥盆世地层出露完好，层序清楚，化石丰富。本文就该剖面法门阶牙形刺动物群、泥盆系石炭系的界线进行了研讨，建立了该区法门阶的两个浅水相牙形刺生物组合带。