On the general character of coastal flow     

Roger L. Hughes 《Pure and Applied Geophysics》1990,133(4):665-689

It is well-known that some coastal currents such as the Florida Current have a recirculating region on their coastal side, while other currents such as the East Australian Current have no such region. Under the hypothesis that the form drag on a coastal current by an irregular coastal topography reduces the momentum transport of the current to a minimum for the given flow within the current, the hydraulic theory of coastal currents is used to explain this behaviour.  相似文献   

Characteristics　and　analysis　of　the　geomagnetic　variations　in　regions　around　the　Qiongzhou　Strait     

范国华  姚同起  顾左文  朱克佳  陈伯舫  冯戬云 《地震学报(英文版)》1994,(2)

Ｃｈａｒａｃｔｅｒｉｓｔｉｃｓ　ａｎｄ　ａｎａｌｙｓｉｓ　ｏｆ　ｔｈｅ　ｇｅｏｍａｇｎｅｔｉｃ　ｖａｒｉａｔｉｏｎｓ　ｉｎ　ｒｅｇｉｏｎｓ　ａｒｏｕｎｄ　ｔｈｅ　Ｑｉｏｎｇｚｈｏｕ　Ｓｔｒａｉｔ（范国华）（姚同起）（顾左文）（朱克佳）（陈伯舫）（冯戬...  相似文献   

首都圈地区地震活动的分期与分区研究     

孙士宏 《地震》1994,(6):19-25

本文通过对首都圈地区（北纬３８．５°至４１．０°，东经１１３．０°至１２０．０°）公元１５００年以来Ｍ≥５地震的系统分析，并应用７０年代以来所取得的该地区最新地球物理场的有关资料进行分区后，发现该地区５级以上地震存在较明显的成组发生及有１１年的时段性特征，且每一组的活动具有地区性特征。这一现象对首都圈地区５级以上的地震的监视预报具有一定的意义。  相似文献   

极隙区粒子和电流的观测和研究     

陈耿雄  徐文耀 《地球物理学进展》1994,9(3):21-36

处于高纬向日面的极隙区是太阳风能量、动量和质量可以直接进入地球磁场并到达地球的近地空间的区域。本文简要介绍了极隙区的观测和研究，综述了极隙区的粒子沉降、场向电流、等离子体对流和电离层电流的特征。  相似文献   

磁层系统的能量输入、输出与日地耦合     

资民筠  沈长寿 《地球物理学报》1994,37(Z2):1-8

用１９７８年和１９８２年３６个磁暴期间的太阳风、行星际磁场（ＩＭＦ）和地磁资料，分析和检验已有的两类太阳风－磁层能量耦合函数．结果表明：Ａｋａｓｏｆｕ提出的耦合函数ε能大致地预报亚暴和磁暴的发生。ε开始起重要作用时即出现亚暴；电离层能耗达到饱和值是发生磁暴的标志。ε与磁层体系能耗之间有接近于对数量的线性关系．用１９７８－１９８６年的资料，分析环电流和极光区电离层能耗在１２１个太阳自转周内的分布表明，日面上可能存在相对持久的活动区域  相似文献   

对可控硅调压整流电路若干问题的分析     

朱厚荣 《武汉大学学报(信息科学版)》1989,(2)

本文比较了两种可控硅整流电路,在这两种电路中把反并联可控硅接入阳极变压器。文章介绍了电路的过压和过流的保护方法并给出了电路的计算公式和经验数据。  相似文献   

对反向变分流电法勘探原理的剖析     

Fu Liangkui 《地球科学》1986,(2)

本文阐明了反向变分流系统地下电流的分布特点和规律。文中还给出了反向变分流电阻率法视电阻率的异常表达式,计算了装置系数和电流分配系数之间的关系,并阐明其规律和作用。最后,作为一个例子,分析了水平地层上反向变分流电测深法视电阻率的异常分布规律,并指出它在勘探中的作用。  相似文献   

The Chemical Composition of Global Subducting Sediments and Its Geological Significance     

Renjie Zhao  Quanshu Yan  Haitao Zhang  Yili Guan  Zhenmin Ge  Long Yuan  Shishuai Yan 《地球科学进展》1986,35(8):789-803

Subducted sediments play an important role in crust-mantle interaction and deep mantle processes, especially for subduction zone magmatism and mantle geochemistry. The current rate of Global Subducting Sediments (GLOSS) is 0.5~0.7 km³/a. The GLOSS are composed of terrigenous material(76 wt.%), calcium carbonate(7 wt.%), opal(10 wt.%) and mineral-bound H₂O⁺(7 wt.%). The chemical compositions of GLOSS are similar to those of upper continental crust which is mainly controlled by the terrigenous materials, and yet the materials formed by marine processes will dilute the terrigenous materials. The components of subducted sediments are different among trenches. In the accretionary margin, the components of subducted sediments are similar to those of the upper crust, while in the non-accretionary margin the components are terrigenous materials plus those produced by marine processes. During subduction, subducted sediments will released fluids, melt or supercritical fluid to affect island arc/back-arc basin magmatism by means of aqueous fluid or sediment melt. In addition, a part of subducted sediments, together with underlying altered oceanic crust/lithosphere, recycle into the mantle and contribute to the mantle heterogeneity. Geochemical tracers indicate that subducted sediments play variable contributions to the magmatic processes in different tectonic setting. Thus, subducted sediments play an important role in two relatively independent dynamics systems (plate tectonics and mantle plume), as well as related mantle evolution models. As a result, by accurately calculating the compositions of subduction sediments and using various geochemical indicators, we can further limit the input and output fluxes of various elements or isotopes, and then obtain more accurately residual subducted components, which can provide us some important clues for geodynamic process.  相似文献   

台风移动规律的研究 Ⅱ.小地形与边界层的动力作用   总被引：1，自引：1，他引：1  

贺海晏  杨平章 《热带气象学报》1995,11(2):97-105

从支配台风中心移动的基本方程出发，着重分析了小地形（地形高度与台风系统的的垂直厚度相双为小量）的抬升作用和边界层的摩擦作用对台风移动影响的定性特征。结果表明，较高地势对台风有“吸收”作用；边界层摩擦辐合引起的艾克曼抽吸有利于台风产生沿局地流场引导速度方向的加速度。  相似文献   

地震系统文献资源的现状及其发展对策     

梁凯利  赵小倩 《国际地震动态》1995,(2):14-17

本文概述了地震系统文献资源的现状及其发展对策，内容包括地震文献资源概况、地震文献资源的调查分析、地震系统文献资源建设中存在的主要问题以及地震文献资源建设发展对策。  相似文献