基于跳跃时间和幅度的BDI指数波动幂律分布特性研究

BDI指数是国际航运市场的风向标,摸清BDI指数波动幂律分布特性,对于进一步掌握运费规律、预测BDI趋势、协助航运决策等方面具有重要意义.基于此,本文对已运行30年BDI指数的波动幂律分布特性进行了详细研究,主要特色有:一是借助Pareto、Exponential以及Fokker-Planck函数首次深入探讨了BDI指数波动幂律分布特性.二是在跳跃识别的基础上,构建了基于跳跃时间和跳跃幅度两标度的BDI指数波动幂律分布特性分析模型,并转化成最小二乘法的线性回归测算模型.三是对BDI指数日、周和月增长率的跳跃时间和跳跃幅度幂律分布特性进行了实证分析.结果表明:BDI指数具有尖峰薄尾的增长率分布和波动聚集性;Fokker-Planck函数拟合BDI指数增长率跳跃时间更合适;Exponential函数拟合BDI指数增长率跳跃幅度更合适;BDI指数增长率跳跃时间和跳跃幅度都具有薄尾幂律特性,且向上、向下幂律呈现对称性.     

新旧《高新技术企业认定管理办法》对比及实施效果分析

针对旧《高新技术企业认定管理办法》及实施过程中出现的问题,2008年4月14日,我国正式颁布实施新管理办法。新《办法》的出台,进一步理清了高新技术企业认定条件,并对认定标准做出了详细说明。通过梳理新旧管理办法运行机制,阐述了新旧管理办法的区别,并对新《办法》实施效果进行深入分析。     

一种基于样本块的图像超分辨率方法研究

提出了一种在马尔科夫网络框架下基于样本块的图像超分辨率算法。算法根据相似性选取多个样本块作为图像重建的候选,在候选集中计算图像块先验概率和图像块之间的相容性,最后在马尔科夫框架下选取最优图像块,合成最终的高分辨率图像。实验证明本文提出的算法具有较好的超分辨率效果。     

BUF634在高频滤波器中设计方法的实现与改进

本文介绍了某型飞机机载高频滤波器的设计方法与工作原理,在此基础上对芯片BUF634的使用方法进行了阐述,并对实际应用中存在的问题进行分析,提出了改进方法。实验验证证明,该方法简单有效,适用范围广。     

QGrid:一种空间移动对象并行索引结构

为提高空间移动对象数据更新效率和查询准确率,提出了一种空间移动对象并行索引结构.利用主索引和辅助索引支持对空间对象进行基于范围的查询和基于对象标识的查询,还通过查询索引将更新操作和可能受其影响的查询操作相连接,在满足并行操作时间片语义的同时,避免了传统方法进行范围查询时对查询范围内相关对象及相关索引结构全部进行锁定的需求.实验结果表明:高负载环境下,该索引结构不但能保证查询准确率,其处理能力也明显优于传统索引结构.该索引通过提高系统并行度,使同一范围内的更新和查询操作可以并行执行,提升了系统整体运行效率.     

白腹锦鸡雌鸟繁殖期的活动区和栖息地选择

2006年3-9月,利用无线电遥测技术和系统搜索法对四川省石棉县栗子坪自然保护区白腹锦鸡雌鸟的繁殖期活动区和栖息地选择进行了研究.对遥测时间超过4个月的3只雌性个体的研究表明:白腹锦鸡雌鸟的繁殖期活动区面积为(31.16±26.02) hm2,核心区面积为(10.06±8.47) hm2;繁殖鸟的活动区在产卵前后有明显变化,算术中心距离超过300 m,未繁殖鸟不明显.白腹锦鸡雌鸟主要选择较稀疏、稍矮、盖度较大、倒木数少的乔木环境和较密而盖度较大的灌木、草本植物的环境.     

包含广义逆的算子乘积的一些不变性

目的给定3个算子A,B和C,推广了Jürgen Groβ和Yongge Tian在文献Invariance properties of a triple matrix product involving generalized inverses([1]Linear Algebra Appl,2006,417:94-107)中得到的主要结论。方法应用算子分块矩阵的技巧和解算子方程的思想进行推导,这与Jürgen Groβ和Yongge Tian的方法完全不同。结果得出了文献[1]的主要结论在无限维Hilbert空间中成立的充要条件。结论得到了与X选取无关的3个算子AXC乘积的一些不变性质,其中X是算子B的不同种类的广义逆。     

末制导雷达干扰技术的系统仿真设计

在分析几种常见末制导雷达干扰技术实现过程特征的基础上,获得具有一定普适性的仿真场景抽象,提出了一种针对单脉冲末制导雷达干扰技术对抗仿真系统构建方法,给出了仿真实现的总体框架,并对具体实现过程中的位置更新、坐标变换、回波产生、波束调制等关键问题进行了论述.使用该方法,构建了多假目标拖引欺骗干扰仿真系统,对该干扰样式实现的主要参数进行了设计,并以距离拖引为例进行了验证.仿真结果验证了该仿真系统构建方法的正确性和有效性.     

Compact fiber-optic diode-laser sensor system for wide-dynamic-range relative humidity measurement

A compact fiber-optic diode-laser sensor system for measuring relative humidity is studied. In such a system, a distributed feedback laser lasing near 1877 nm is used as light source while a high-precision Pt resistance as temperature sensor, an accuracy of 0.1% relative-humidity can be achieved. The laser sensor system is able to lock to the absorption peak and calculate the density of water vapor without any additional reference measurements. Using programs built in to the microcontroller unit, the laser system can switch functions between direct measurement at high density and second-harmonic detection at low density. The system can switch between the two modes automatically and work in a wide dynamic range.     

A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co,southern Tibet

A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue samples were selected, and organic carbon stable isotopes were obtained using the AMS ¹⁴C chronological method. The ¹⁴C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using ²¹⁰Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian monsoon during the Holocene.