中国2003年北极海冰调查及未来北极海冰研究战略

以建立气候模式中的海冰模式为主线 ,首先回顾了国际上海冰模式发展现状和趋势 ,从现有模式机理上存在的问题说明认识海冰各物理过程的现场和实验室调查研究的关键科学问题。之后介绍了中国第二次北极科学考察中的海冰调查内容。最后结合国内调查研究能力和国际上海冰科学发展走向 ,根据国内外资料和极地海冰的客观现象 ,提出 6项战略 ,希望作为以后中国北极海冰理论和模式为背景的现场和实验室研究的方向。     

北极大气边界层初步模拟试验

应用一维K闭合OSUPBL模式和ARCSCM极地柱模式,采用SHEBA观测资料和ECM- WF的输出结果作为模式的初始场和外强迫场,对SHEBA试验所在地(75°N,150°W)单点的北极大气边界层特征,进行了初步的模拟并与SHEBA资料进行对比分析。研究表明,这两个模式都具有较好地模拟单点北极大气边界层特征的能力。OSUPBL模式在垂直高度上的高分辨率,使其能够更好地反映大气边界层内部的细微变化特征。ARCSCM模式中考虑了比较多的物理过程,且需要提供比较完整的初始场、边界条件和侧向强迫,并每小时更新,模拟结果更符合实际情况。对模式的不足和下一步的研究也进行了讨论。     

喀拉海峡潮-地相互作用激发非线性内波的数值模拟

Nonlinear internal waves(NIWs) are ubiquitous around the Kara Sea, a part of the Arctic Ocean that is north of Siberia. Three hot spot sources for internal waves, one of which is the Kara Strait, have been identified based on Envisat ASAR. The generation and evolution of the NIWs through the interactions of the tide and topography across the strait is studied based on a nonhydrostatic numerical model. The model captures most wave characteristics shown by satellite data. A typical inter-packets distance on the Barents Sea side is about 25 km in summer, with a phase speed about 0.65 m/s. A northward background current may intensify the accumulation of energy during generation, but it has little influence on the other properties of the generated waves. The single internal solitary wave(ISW) structure is a special phenomenon that follows major wave trains, with a distance about 5–8 km. This wave is generated with the leading wave packets during the same tidal period. When a steady current toward the Kara Sea is included, the basic generation process is similar, but the waves toward the Kara Sea weaken and display an internal bore-like structure with smaller amplitude than in the control experiment. In winter, due to the growth of sea ice, stratification across the Kara Strait is mainly determined by the salinity, with an almost uniform temperature close to freezing. A pycnocline deepens near the middle of the water depth(Barents Sea side), and the NIWs process is not as important as the NIWs process in summer. There is no fission process during the simulation.     

打通海洋信息资源“大动脉” 推进海洋信息化进程——《关于进一步加强海洋信息化建设的若干意见》解读

"信息孤岛、分散管理、业务难协同"是当前制约海洋信息化向纵深发展的主要问题。为从根本上解决国家海洋信息化工作中面临的这些深层次问题,国家海洋局信息化工作领导小组统筹考虑,谋篇布局,提出了打造海洋信息通信"一张网"、国家海洋信息资源"一朵云"、海洋政务服务"一个平台"、海洋管理决策"一片海"的"四个一"系统工程,并向国家海洋局系统和沿海省、市、自治区海洋主管部门印发了《关于进一步加强海洋信息化建设的若干意见》。该意见对优化海洋信息化发展环境,增强海洋信息化发展能力,提高海洋信息化应用水平,破解国家海洋局信息化建设中的突出问题,全面推进海洋信息化建设工作具有重要指导意义。     

Electron impact excitation rate coefficients of N II ion

This paper calculates the electron impact excitation rate coefficients from the ground term 2s²2p^{2 3}P to the excited terms of the 2s²2p², 2s2p³, 2s²2p3s, 2s²2p3p, and 2s²2p3d configurations of N II. In the calculations, multiconfiguration Dirac--Fork wave functions have been applied to describe the target-ion states and relativistic distorted-wave calculation has been performed to generate fine-structure collision strengths. The collision strengths are then averaged over a Maxwellian distribution of electron velocities in order to generate the effective collision strengths. The calculated rate coefficients are compared with available experimental and theoretical data, and some good agreements are found for the outer shell electron excitations. But for the inner shell electron excitations there are still some differences between the present calculations and available experiments.     

论河南地理研究事业的发展

以学术总结为主要线索,系统分析了４０年来河南地理研究的三大发展阶段及其重点研究了内容,评价了河南地理研究在ＧＩＳ,软件学和地理学应用技术与开发三大领域的现状特点,提出了未来河南地理研究的重点是抓好人才工程,计算机工程,名牌战略工程。     

交互实至波检测与表层模型正反演

初至波表层速度模型层析反演是层析静校正的重要基础,作者研究了一套完整的方法和软件系统,利用计算机可视化技术进行人机交互初至波检测、表层模型正演及反演,可直观地分析、监控初至波检测的合理性及模型层板反演的质量,提高表层速度模型层析反演的可靠性,为层析静校正提供合理的表层速度模型。     

边坡加固中预应力锚索地梁极限状态设计方法

根据预应力锚索地梁加固边坡工程的特点,对预应力锚索地梁的不同工作阶段和受力状态进行了详细分析,在此基础上提出了一种锚索地梁的极限状态设计方法,给出了其具体计算过程。应用该方法对某工程实例进行了计算,计算结果的对比分析表明,当锚索进入极限工作状态时对地梁进行极限状态的设计是必要的。     

湟源地区新的春旱指标的确定和冬灌效应分析

本利用湟源１９５１－１９９５年降水和气温资料,分析了湟源地区气候变化特征,建立了包含温度和上年秋季降水条件的新的春旱评估指标,并就冬灌对春小 麦产量形成的影响效应进行了简要分析。