基于Android的移动气象信息传输监控软件开发

介绍如何利用Mono for Android、ASP.NET、C#开发一套可以在智能手机上使用的上行气象信息传输实时监控软件,以保障上行气象信息的时效性。从软件的需求分析、软件架构、软件实现等方面阐述了如何在技术上安全、及时、准确的实现对气象信息传输情况的实时监控,并对主要功能的实现与优化进行了详细介绍：通过Web Service技术获取、发布传输监控信息、进行用户权限控制,优化Web Service性能,以保障监控信息安全、高效的传输;利用后台服务、隐式线程、定时警报实现快速响应、节约系统开销的手机客户端;构建兼容性、独立于分辨率的UI。     

基于Android的数据调绘系统

一体化数据调绘系统在生产中有着重要的作用。结合数据组织和数据库加密关键技术,对Android下数据调绘系统实现与应用进行了研究。开发完成原型系统,满足了爱尚重庆POI调绘需要。     

在线巡查技术在土地变更调查中的应用研究

在线巡查技术是指巡查人员通过移动终端连接服务器在线交互数据的一项技术,是近年来逐步发展应用于土地执法较为成熟的技术,对于需要外业调查以及室内审核的项目同样具有很好的应用效果。随着技术和装备的不断更新,全国土地变更调查工作也在提出新的要求,为适应新的形式,广东省首次利用已建成的省级在线巡查系统辅助开展县(市、区)土地变更调查,本文对省级在线巡查系统设计模式应用于土地变更调查工作进行了深入的分析和研究。     

基于Android平台的地震灾情采集系统的设计与实现

震后及时准确的灾情信息,可为应急救援力量部署、应急指挥决策和地震烈度评定提供重要依据。分析震后第一时间多方面地震现场灾情的实际需求,基于Android平台的地震现场灾情采集系统的研发目标,分析系统的业务流程,进行系统架构设计和系统客户端、中间层和数据层设计,详细描述灾情信息和烈度上报、查询管理、统计分析等功能的实现,功能测试结果展示该系统的适用价值和灾情采集效率。     

面向飞行器可视导航的复杂空地环境动态3维表示模型

针对飞行器可视导航中复杂空地环境时空要素统一精准表示的难题,本文提出了面向飞行器可视导航的复杂空地环境动态3维表示的GIS数据模型和相应的时刻数据存储结构,并用UML图进行了描述。该模型综合考虑了复杂空地环境要素多维、动态、边界模糊等特点,刻画了多维动态时空数据在空间、时间、尺度、语义四个方面的特征及其相互关系。最后,以某机场的空地环境数据的组织、分析和可视化为例,验证了该模型的实用性。     

ON THE EFFECT OF AMBIENT TURBULENCE ON THE BUOYANT PLUME RISE

Considering the effects of both entrainment and intensification of the exchanges of momentum and heat between plume and ambient air,we have derived the trajectory equation of buoyant plume under neutral conditions,and the final rise prediction formula theoretically without any hypotheses on the rise termination.Compared with the field experiments,the final rise formula simulates the observed final rise heights well.     

天气雷达数字化终端及其应用软件

为解决雷达数据采集、实时显示、数据存储、资料处理自动化等问题，进行了天气雷达数字化终端和应用软件技术的研究和开发。改变了711B-1雷达数据存储、分析自动化程度低的状况。增加和丰富了雷达二次产品，使雷达资料得到了充分的分析和应用，提高了雷达对天气的监测能力。增加了对冰雹、暴雨等强对流天气的预警功能、人工增雨效果检验等功能。     

Long-term investigation of benthic fauna and the influence of treated ballast water disposal in Port Valdez,Alaska

Benthic faunal structure and hydrocarbon concentrations in sediments were examined annually for 10 years (1989-1998) in Port Valdez, Alaska, where a near-bottom permitted discharge of treated tanker ballast waters containing residual petroleum has occurred since 1977. Measured concentrations of hydrocarbons in sediments near the discharge showed detectable increases in concentration, but on only one occasion were these increases either to levels exceeding ecotoxicological thresholds (Effects-Range Low, ER-L) or associated with alterations in the benthic community. Changes in faunal structure indicating disturbance were observed at one station near the discharge from 1995 to 1997 and were apparent as increased numbers of opportunistic taxa and anomalous trends in abundance and diversity. Minimum-effect (ME) hypotheses provided evidence of negligible to small effects on benthic infauna from disposal of treated ballast water. ME hypotheses have the potential to assist both researchers and managers by providing a tool to relate scientific results to ecological importance and decision criteria.     

计量用水智能监测系统的设计与实现

水位传感器与单片机智能遥测终端相配合设计的计量用水智能监测系统可以通过电话线，将计量用水信息远程数传到监控中心，并在监控中心生成各种图文、报表。通过对图文、报表的分析，实现对智能遥测终端的远程监控。该系统将在水利建设中发挥重要作用。     

Variable style of transition between Palaeogene fluvial fan and lacustrine systems, southern Pyrenean foreland, NE Spain

Two Palaeogene fluvial fan systems linked to the south‐Pyrenean margin are recognized in the eastern Ebro Basin: the Cardona–Súria and Solsona–Sanaüja fans. These had radii of 40 and 35 km and were 800 and 600 km² in area respectively. During the Priabonian to the Middle Rupelian, the fluvial fans built into a hydrologically closed foreland basin, and shallow lacustrine systems persisted in the basin centre. In the studied area, both fans are part of the same upward‐coarsening megasequence (up to 800 m thick), driven by hinterland drainage expansion and foreland propagation of Pyrenean thrusts. Fourteen sedimentary facies have been grouped into seven facies associations corresponding to medial fluvial fan, channelized terminal lobe, non‐channelized terminal lobe, mudflat, deltaic, evaporitic playa‐lake and carbonate‐rich, shallow lacustrine environments. Lateral correlations define two styles of alluvial‐lacustrine transition. During low lake‐level stages, terminal lobes developed, whereas during lake highstands, fluvial‐dominated deltas and interdistributary bays were formed. Terminal lobe deposits are characterized by extensive (100–600 m wide) sheet‐like fine sandstone beds formed by sub‐aqueous, quasi‐steady, hyperpycnal turbidity currents. Sedimentary structures and trace fossils indicate rapid desiccation and sub‐aerial exposure of the lobe deposits. These deposits are arranged in coarsening–fining sequences (metres to tens of metres in thickness) controlled by a combination of tectonics, climatic oscillations and autocyclic sedimentary processes. The presence of anomalously deeply incised distributary channels associated with distal terminal lobe or mudflat deposits indicates rapid lake‐level falls. Deltaic deposits form progradational coarsening‐upward sequences (several metres thick) characterized by channel and friction‐dominated mouth‐bar facies overlying white‐grey offshore lacustrine facies. Deltaic bar deposits are less extensive (50–300 m wide) than the terminal lobes and were also deposited by hyperpycnal currents, although they lack evidence of emergence. Sandy deltaic deposits accumulated locally at the mouths of main feeder distal fan streams and were separated by muddy interdistributary bays; whereas the terminal lobe sheets expand from a series of mid‐fan intersection points and coalesced to form a more continuous sandy fan fringe.