电离层GPS掩星反演技术研究   总被引：5，自引：3，他引：2       下载免费PDF全文

林剑  吴云  刘经南 《地球物理学报》2009,52(8):1947-1953

GPS无线电掩星技术是崭新的、高效的地球大气层和电离层探测技术,但仍在发展和完善之中.本文详细推导了Abel积分和绝对TEC电离层反演方法,研究了如何解决Abel积分产生的上下限异常问题;用COSMIC发布的GPS原始数据进行了反演计算,将结果与地面电离层测高仪数据进行了比较,最后讨论了周跳对反演结果的影响问题.结果表明：（1）在较高轨道高度（约800 km）,Abel积分与绝对TEC方法的反演结果基本一致,都与电离层测高仪反演结果符合良好;在较低轨道高度（约500 km）,绝对TEC反演精度优于Abel积分反演精度;（2）绝对TEC反演的最大电子密度N_m较Abel积分法获得的结果更接近于电离层测高获得的峰值电子密度N_mF₂,绝对TEC反演法更加严密和有效;（3）周跳对绝对TEC反演结果的影响较Abel积分反演结果的影响更为敏感,但无论哪种方法,周跳对反演精度都造成严重损失.综合而言,绝对TEC反演法是更优的方法.  相似文献   

Dating Methods of Cold-water Corals and Their Application in Reconstructing Carbon-reservoir Ages of Intermediate and Deep Oceans     

Enqing Huang  Le Kong  Jun Tian 《地球科学进展》2019,34(12):1243-1251

Establishing a precise chorology is a critical issue when employing cold-water coral as paleoenvironmental archives. Currently, U-Th, ¹⁴C and ²¹⁰Pb dating techniques are the most frequently used methods. The high-magnesium calcite skeleton of bamboo coral has clear growth bands, which is appropriate for ¹⁴C and ²¹⁰Pb dating methods and holds a great potential to be high-resolution archives of mid-to-deep ocean evolution. Aragonitic stony coral is appropriate for both U-Th and ¹⁴C dating methods, which is valuable in paleoceanographic research. Because the U-Th method can provide the absolute chronology of coral samples, it can further be used to calculate the ¹⁴C age of ocean carbon reservoirs. Therefore, U-Th and ¹⁴C dating results of stony coral are currently the most reliable data for exploring the evolution of ocean carbon reservoirs through the Last Glacial Maximum to the present. It has been found that the ¹⁴C ventilation ages of intermediate water masses of the equatorial Atlantic and Southern Ocean significantly decreased at the end of the Heinrich Stadial 1. This suggests a massive carbon transfer from deep oceans to the atmosphere, or the Atlantic intermediate depths were ventilated by the southern- and the northern-sourced water masses, respectively, before and after the Heinrich Stadial 1.  相似文献   

Cycle Slip Detection and Ambiguity Resolution Algorithms for Dual-Frequency GPS Data Processing   总被引：13，自引：0，他引：13  

Yang Gao  Zuofa Li 《Marine Geodesy》1999,22(3):169-181

This article investigates the problem of cycle slip detection and ambiguity resolution using dual-frequency GPS data. Several algorithms are proposed and described. F or cycle slip detection, three L1/L2 observable combinations have been integrated to formulate a new algorithm for cycle slip detection. For ambiguity resolution, both widelane and narrowlane ambiguity resolution algorithms are presented, but the focus is on the narrowlane ambiguity resolution. Numerical results are included to evaluate the performance of the proposed algorithms, which have shown that cycle slips can be effectively detected and the narrowlane ambiguities can be resolved almost instantaneously after successful determination of the widelane ambiguities.  相似文献   

磷循环的非线性动力学特性及富营养化     

韦海英  柴立和 《湖泊科学》2006,18(6):557-564

本文在假设湖泊受单一营养盐磷限制和不考虑湖底沉积物影响的情形下,建立了一个单层箱体磷循环的非线性动力学模型,研究湖泊中颗粒磷、可溶性磷和藻类中的磷这三种磷之间的相互关系,理论上分析了磷循环系统的稳定特性,得出三种形式的磷共存是系统趋向稳定的平衡点．然后论文又从人工治理的角度,通过数值计算综合考虑外源性磷、水力冲刷、生物调控和基质浓度因素对磷循环的影响,分析不同因素的改变对系统和湖泊水质的影响,进而对这一类的富营养化现象防治提供可行性的工程上的实际建议．  相似文献   

中央造山带的演化及其特点   总被引：105，自引：12，他引：93  

殷鸿福  张克信 《地球科学》1998,23(5):437-442

中央造山带原型是由一列微板块加上分别位于其北面和同面的两列不同时期的小洋盆组成,微板块群的主体是柴达木,秦岭,大别－苏鲁,还加上祁连,元古代末至早古生代早期,北列拉张成多岛小洋盆,它们在加里东档期关闭,并在微板块群北缘形成前陆盆地带,南列形成裂陷槽,在加里东期末关闭,一般不造山,晚古生代,微板块群与欧亚板块合为一体,并总体北移,南列出现泥盆（个别）石炭二叠纪的小洋盆,属于古特提斯洋的一部分,洋盆在  相似文献   

云南金平勐拉峨眉山玄武岩型铜矿矿化规律   总被引：1，自引：0，他引：1  

杨昌毕  王明聪 《云南地质》2012,(2):177-181,158

赋矿的峨眉山玄武岩系以爆发相角砾状玄武岩为底,沉积相凝灰岩为顶,可明显划分为三大火山喷发旋回和三岩性段,每一喷发旋回分别对应Ⅰ、Ⅱ、Ⅲ铜矿化层,喷发旋回与铜矿(化)体(层)间存在明显的对应关系,工业矿体由后期含矿构造热液叠加再富集而成。  相似文献   

Neoproterozoic SHRIMP U–Pb zircon ages of silica-rich Dokhan Volcanics in the North Eastern Desert,Egypt     

Christoph Breitkreuz  Hassan Eliwa  Ibrahim Khalaf  Khaled El Gameel  Benjamin Bühler  Sergei Sergeev  Alexander Larionov  Mamoru Murata 《Precambrian Research》2010

Chronology of Neoproterozoic volcanosedimentary successions remains controversial for many regions of the Arabian–Nubian Shield, including the Dokhan Volcanics of NE Egypt. New U–Pb zircon SHRIMP ages have been obtained for 10 silica-rich ignimbrites and two subvolcanic dacitic bodies, mapped as Dokhan Volcanics, from the North Eastern Desert of Egypt. Crystallization ages range between 592 ± 5 and 630 ± 6 Ma (Early Ediacaran). Apparently, the late consolidation of the Arabian–Nubian Shield was accompanied by the evolution of isolated volcanic centres and basin systems which developed during a period of approx. 40 Ma, independently in space and time and probably under changing tectonic regimes. The obtained age data together with other previously published reliable ages for Dokhan Volcanics suggest two main pulses of volcanic activity: 630–623 Ma and 618–592 Ma. Five samples contain inherited zircons, with ages of 669, 715–746, 847 and 1530 Ma, supporting models that North Eastern Desert crust is mainly juvenile Neoproterozoic crust.  相似文献   

卫星资料循环同化应用对区域数值预报效果影响分析   总被引：1，自引：1，他引：0  

刘君  黄江平  董佩明  张文军  严仕尧  张长国 《气象》2013,39(2):156-165

为提高卫星资料在同化系统中的利用率及验证卫星微波资料对区域数值预报效果的影响,本文以2008年8月1-31日为研究时段,利用WRF模式及其WRF-3DVAR同化模块,设计并构建了卫星微波资料的快速循环同化方案,分析循环同化方案对数值预报的改进效果.结果表明,相比于单时次同化,循环同化方案使各预报要素的相关系数在一定程度上得到改善,均方差也呈现减小的趋势.此外,对研究时段内暴雨和台风个例的具体分析显示,循环同化方案能够有效改善降水和台风路径的预报.  相似文献   

The Cambrian to Aquitanian geological record of the Longi-Taormina Unit (Calabria-Peloritani Arc,southern Italy): geodynamic implications     

《Geodinamica Acta》2013,26(6):417-430

The Longi-Taormina Unit forms the “Dorsale calcaire” of the Peloritani Alpine Belt (southern Calabria-Peloritani Arc). It is made by a thick sedimentary cover of Meso-Cenozoic age overlying a Variscan weakly metamorphosed Cambrian to Carboniferous succession.

The Palaeozoic series consists of pelitic to arenaceous sediments containing layers of acidic and basic volcanics. The acidic volcanics are affected by the “Caledonian” compressional deformations and are referred to Early Ordovician. The basic rocks belong to two different volcanic cycles; the first, not dated, is ascribed to the Caledonian cycle according to its geochemical signature; whereas the second, middle-late Devonian in age, is interpreted to have formed in the framework of pre-Variscan extensional tectonics. During the Variscan Orogeny (330 Ma), the area recorded metamorphism up to subgreenschist-to-greenschist facies and two main deformation phases, marked by syn-schistose early folds (Dv₁), overprinted by dominantly NW-SE trending late folds (Dv₂).

During the Aquitanian, deformation related to the Alpine Orogeny led to imbrication of the Palaeozoic and Meso-Cenozoic series. The sedimentary cover was affected by a series of N090° to N130° trending folds. Detailed stratigraphical and structural investigations on the tectonic contact between the Longi-Taormina Unit, and the overlying Fondachelli Unit indicate that this structure is part of a frontal thrust ramp which developed during the Aquitanian.

Our geological and structural studies on the Cambrian to Aquitanian rocks of the Longi-Taormina Unit of the Calabria-Peloritani Arc enable to unravel the complex geodynamic history of the central-western Mediterranean area.  相似文献   

辽东半岛四堡旋回地质作用及其构造意义——以辽东榆树砬子组为例   总被引：2，自引：0，他引：2  

于海峰  董万德  何振清  郝永利  谭文刚 《地质与资源》2010,19(3):224-229

建立在岩石组合、变质、变形和同位素年代学基础上的研究成果表明,辽东半岛榆树砬子组是经历了绿片岩相浅变质的滨浅海相单陆屑碎屑岩含铁建造,其时代应归属中元古代.在下伏辽河群褶皱回返之后上覆永宁组堆积之前其经历了四堡旋回构造变形,并与四堡旋回末期快速堆积的永宁组共同构成中间构造层,使得辽东地区地壳具多元化的三层式结构.  相似文献