格形编码的正交频分复用技术在时间色散信道中的应用

提出了一种格形编码的正交频分复用 (TC OFDM )方案 ,研究把正交频分复用(OFDM )和格形编码 (TCM )有机地结合 ,来克服时间色散信道中的频率选择性和多径衰落。对码率 2 / 3格形编码的 8DPSK OFDM在时间色散信道中的误码率性能进行了分析和模拟 ,讨论了不同正交载波数情况下格形编码的设计。结果表明 ,在比特误码率BER为 10 - 3时采用TC OFDM方案与未编码系统相比可以提供 6dB的编码增益。     

OFDM基带处理系统的设计与实现

阐述了适合高速无线数据传输的正交频分复用(OFDM)调制方式的基本原理及调制解调的快速傅立叶变换(FFT)实现,并给出OFDM基带处理系统的结构图和硬件模块框图。     

选择映射法降低OFDM系统的峰均比

正交频分复用（OFDM）系统的一个主要缺点是峰均功率比（PAPR）过高.选择映射法（SLM）是一种有效的降低OFDM系统的峰均功率比的方法.采用一种改进的选择映射法,把降低峰均功率比和信道编码相结合.仿真结果表明,不仅能够降低OFDM系统的峰均比,而且系统的误比特性能也得到提高.     

基于导频序列的OFDM信道估计性能分析

正交频分复用(OFDM)作为一种可以有效对抗符号间干扰(ISI)的高速传输技术,得到了广泛的应用,而信道估计技术作为其重要技术之一得到了很大的发展.信道估计分为盲信道估计、半盲信道估计和基于导频的信道估计.主要研究基于导频的最小平方(LS)信道估计和线性最小均方误差(LMMSE,Linear Minimum Mean Square Error)信道估计,在不同的信道环境和不同的循环前缀(CP)和导频子载波数下的性能比较并得出结论.     

跳频技术与同频复用相结合的应用分析

跳频与同频复用是移动通信系统中重要的两种应用技术。简介跳频技术与同频复用的基本原理，并着重分析了在实际应用中跳频与同频复用相结合的几种方式。     

一种高效的迭代OFDM频偏估计算法

提出了一种改进的正交频分复用（Orthogonal Frequency Division Multiplexing,OFDM）载波频率偏移估计算法并通过MATLAB进行仿真.仿真结果表明算法对小数载波频率偏移估计精度高并且其算法复杂度低.     

MIMO OFDM短波无线通信同步技术的研究

多输入多输出（MIMO）技术是最近几年发展起来的无线通信技术。目前利用MIMO技术提高短波通信的传输速率和可靠性的研究已经开展。着重研究了MIMO OFDM（交频分复用）短波无线通信的同步技术，利用截断的Suehiro序列构成的训练符号完成了系统的同步捕获。仿真结果标明，与Mody算法相比，该方案在性能相近的情况下可提高系统的频谱效率。     

海陆一体机载激光扫描仪的设计

提出了海陆一体机载激光扫描仪设计方案。采用高频双波长激光以及大动态接收光路,实现地貌与水深的联合探测;采用基于自校准时间数字转换,重构高精度的点云数据;采用基于编码正交频分复用调制解调技术,实现机载点云探测数据的快速回传。     

基于RS码跳频序列的一种编写方法与实现

跳频通信是一种有效的抗干扰通信技术，跳频序列的性能对跳频通信系统的性能有着决定性的影响。重点阐述了RS码作为跳频序列的编码方法及其性能，介绍了RS码序列的具体编写方法，并进行了计算机仿真，计算了所生成RS跳频序列的汉明相关性能。     

汶东凹陷古近纪地层特征及沉积环境分析

汶东凹陷古近系分为古新世固城组和始新世大汶口组。大汶口组又分上、中、下3段，相应有3个化石组合带。从地震反射看，该凹陷内自下而上呈5组反射波特征。以古近纪地层特征为基础，结合构造演化分析认为：固城组为干旱气候条件下的山麓洪积相沉积，大汶口组下段为干旱条件下浅湖相沉积，大汶口组中段为逐渐湿润条件下的氧化一还原湖相沉积，大汶口组上段为潮湿气候条件下的还原湖相沉积。     

Thermohaline structure inhomogeneity associated with polynia at the northern margin of Emery Ice-shelf

Based on the hydrographic data in austral summer during the 22nd Antarctic Expedition of China(2005/2006),some features can be found about the northern margin of Emery ice shelf as follows.The heat content in the surface layer(0-50 m) at the eastern end and the western end of the ice-shelf margin is much higher than that at the middle.The upper mixing-layer depth and the seasonal thermocline depth at the middle of the ice-shelf northern margin are much shallower than those at the both ends.However there is much less difference between the middle and the ends in the bottom layer.The remote sensing photos show that the inhomogeneity in the surface-layer water is closely related to the spatial distribution of the floes and polynia in the area.     

Phylogenetic analysis of cultivable bacteria isolated from Arctic sea-ice

Phylogenetic analysis based on 16S rDNA of 8 strains of cultivable bacteria isolated from Arctic sea-ice was studied.The results showed that strain BJ1 belonged to genus Planococcus,which was a genus of low mole percent G C gram-positive bacteria;strain BJ6 belonged to genus Burkholderia of β-proteobacteria and the rest 6 strain all belonged to γ-proteobacteria,of which strain BJ8 was a species of Pseudoalteromonas,strain BJ2-BJ5 and BJ7 were members of genus Psychrobacter.Phylogenetic analysis also indicated that bacteria of genus Psychrobacter of the isolates formed a relatively independent phylogenetic cluster in comparison with other bacteria belonged to genus Psychrobacter.     

Foreword

正Rapid changes of Arctic sea ice cover have been in the focus of the international climate research community in recent years.Quite a few of nations have completed a large number of related surveys and research projects in the Arctic Ocean.Up to now,China has performed six research cruises to the Arctic Ocean resulting in a significant volume of research output.Improved knowledge on the atmospheree-sea ice-ocean interactions in the Arctic is a     

Exposure ages and radiogenic ages of ureilite(GRV 024516) and ordinary chondrite(GRV 024517) from Antarctica

The GRV 024516 and GRV 024517 meteorite samples collected from Grove Montains,Antactica are ureilite and H5 ordinary chondrite,respectively.Based on the study of mineralogy-petrology,the cosmic-ray exposure ages and gas retention ages of these two meteorites were determinated and calculated.Their cosmic-ray exposure ages are 33.3 Ma,51.7 Ma,and gas retention ages are 1936.8 Ma and 3720 Ma,respectively.The ureilite contains diamond,graphite and amorphous C,which are mainly carrier of noble gases indicating obviously shock metamorphism effects,which induced 40Ar partial loss.The H5 chondrite indicates thermal metamorphism of parent body,its gas retention age fall the range between 3220 Ma and 4510 Ma of the least shocked H5 chondrites     

Information for authors

正1 Aims and Scope Advances in Polar Science(APS)is an international,peer-reviewed journal jointly sponsored by the Polar Research Institute of China and the Chinese Arctic and Antarctic Administration.APS is a comprchensive academic journal dedicated to presentation of multi-disciplinary achievements in Arctic and Antarctic expeditions and research.Its primary purpose is to publish achievements in fundamental research,applied     

Advances in Polar Science CONTENTS(Volume 25,2014)

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Guide to Authors： Journal of Mountain Science

<正>AIMS AND SCOPE(Editorial Policy)The Journal of Mountain Science(JMS)is devoted to mountains and their surrounding lowlands-ecoregions of particular global importance,with a particular emphasis on the important highlands/mountains in the world,such as the Tibetan Plateau,the Himalayas,the Alps,the Andes,the Rockies and many other mountain ranges of our planet.     

Journal of Mountain Science(JMS)

<正>The Journal of Mountain Science(JMS),founded in2004,is an international English-language journal on mountain sciences.JMS is supervised by the Chinese Academy of Sciences(CAS),sponsored by the Chengdu Institute of Mountain Hazards and Environment,CAS,published by Science Press China,and distributed by Springer exclusively throughout the world(excluding Mainland China).The JMS is published bimonthly,fulltexted in SpringerLink and CNKI,indexed/abstracted by