真实感水面波浪模型算法的研究与实践

研究了虚拟地形环境中3维水面波浪模型的基本建模及效果的实现。同时提出几种不同的海浪模型,重点对规则海浪模型算法进行了研究。为满足显示的实时性,在优化算法的同时,采用计算和显示分开的策略。既满足了显示质量的要求,又满足了大量高精度波浪数据的要求。     

一种微地形探测回波信号处理的新算法

针对钴结壳具体赋存环境和开采技术要求,作者提出了利用Morlet小波信号包络和高斯函数曲线及能量相关性算法对拟设计的微地形探测方法接收到的超声回波信号进行分析与计算。由实验初步验证,利用该算法计算出来的被测对象位置精度及误差稳定性均高于传统的超声波单波束多探头探测方法。     

基于Pocket PC全要素1∶5万GIS数据采集系统

由于国民经济的迅速发展,对国家的基础地理信息数据的时效性需求在不断发生变化。为了保持和维护国家基础地理信息数据库的时效性,需要对其进行及时更新和维护。从我国1∶5万基础地理信息数据库的更新和维护的要求出发,提出了基于Pocket PC的全要素GIS数据采集系统的设计方案,并对全要素地理数据采集中的关键问题进行了讨论。重点提出了基于嵌套链表数据结构的全要素地物属性编码表的管理以及基于面向对象思想的地物属性二次抽象实现技术;对1∶5万基础地理信息中GPS空间数据采集进行了分析,提出了多点平滑的GPS数据处理技术;对外业数据记录进行了分析和讨论;对解决上述问题所开发的并已经应用于1∶5万基础地理信息中GPS空间数据采集系统软件的开发基本思路进行了描述。     

地球重力场可视化数据挖掘平台WHU-3Dgravity的设计与实现

随着地球重力场理论研究的发展,地球重力场的三维可视化成为需要,将数据挖掘技术应用于地球重力场三维可视化是一个新兴的研究领域。为此,提出了地球重力场可视化数据挖掘平台WHU-3Dgravity的设计与实现,并对其关键技术进行了分析。     

Eddy covariance measurements of carbon dioxide,latent and sensible energy fluxes above a meadow on a mountain slope

Carbon dioxide, latent and sensible heat fluxes were measured by means of the eddy covariance method above a mountain meadow situated on a steep slope in the Stubai Valley in Austria, based on the hypothesis that, due to the low canopy height, measurements can be made in the shallow equilibrium layer where the wind field exhibits characteristics akin to level terrain. In order to test the validity of this hypothesis and to identify effects of complex terrain in the turbulence measurements, data were subjected to a rigorous testing procedure using a series of quality control measures established for surface-layer flows. The resulting high quality dataset comprised 36% of the original observations, the substantial reduction being mainly due to a change in surface roughness and associated fetch limitations in the wind sector dominating during nighttime and transition periods. The validity of the high quality dataset was further assessed by two independent tests: (i) a comparison with the net ecosystem carbon dioxide exchange measured by means of ecosystem chambers, and (ii) the ability of the eddy covariance measurements to close the energy balance. The net ecosystem CO₂ exchange measured by the eddy covariance method agreed reasonably well with ecosystem chamber measurements. The assessment of the energy balance closure showed that there was no significant difference in the correspondence between the meadow on the slope and another one situated on flat ground at the bottom of the Stubai Valley, available energy being underestimated by 28% and 29%, respectively. We thus conclude that, appropriate quality control provided, the eddy covariance measurements made above a mountain meadow on a steep slope are of similar quality as compared to flat terrain.     

GML数据的Web可视化设计与实现

GML是GIS领域的通用交流语言,然而目前的浏览器并不支持GML,因此GML的Web可视化仍是GML应用需要解决的问题。为此,本论文提出了一种基于组件的可视化策略。该策略采用文档对象模型(DOM)进行GML模式文件和实例文件解析,按地理要素对GML进行数据分流/分层,然后分层可视化的办法,实现了GML数据的Web可视化。实践验证,该方法是切实可行的,且对于GML数据量较大时尤为有效。     

Detection of a collision zone in south Indian shield region from magnetotelluric studies

Magnetotelluric (MT) investigations were carried out along a profile in the greenschist–granulite transition zone within the south Indian shield region (SISR). The profile runs over a length of 110 km from Kuppam in the north to Bommidi in the south. It covers the transition zone with 12 MT stations using a wide-band (1 kHz–1 ks) data acquisition system. The Mettur shear zone (MTSZ) forms the NE extension of Moyar–Bhavani shear zone that traverses along the transition zone. The regional geoelectric strike direction of N40°E identified from the present study is consistent with the strike direction of the MTSZ in the center of the profile. The 2-D conductivity model derived from the data display distinct high electrical resistivity character (10,000 Ω m) below the Archaean Dharwar craton and less resistive (< 3000 Ω m) under the southern granulite terrain located south of the MTSZ. The MTSZ separating the two regions is characterized by steep anomalous high conductive feature at lower crustal depths. The deep seismic sounding (DSS) study carried out along the profile shows dipping signatures on either side of the shear zone. The variation of deep electrical resistivity together with the dipping signature of reflectors indicate two distinct terrains, namely, the Archaean Dharwar Craton in the north and the Proterozoic granulite terrain towards south. They got accreted along the MTSZ, which could represent a possible collision boundary.