Faure序列的周期性及快速构造     

林鹭 《华东地质学院学报》2003,26(2):113-114

通过分析Faure序列的结构，得到Faure序列的周期性以及模2下Faure序列的快速算法。该算法无需直接写出相关矩阵，仅包含矩阵及向量的逻辑运算和加法运算，不包含乘法运算。  相似文献   

气候演变中的冰和碳   总被引：18，自引：0，他引：18  

汪品先 《地学前缘》2002,9(1):85-93

地质历史上充满着冰盖消长 (“暖室期”和“冰室期” ,“冰期”和“间冰期”)与大气CO2 增减的周期性变化 ,而两者之间的关系并不清楚。由于冰盖变化的地质标志比大气CO2 变化的标志容易认识 ,长期以来古气候研究侧重“冰” ,而对“碳”即碳循环的研究不足 ,通常将碳循环的变化解释为冰盖变化的结果。近年来越来越多的发现表明 ,单纯用水循环的物理过程不能解释冰盖演变的许多现象 ,而且大气CO2 变化往往领先于冰盖。揭示碳循环变化对冰盖演变的影响 ,认识生物地球化学过程在冰期旋回中的作用 ,将不同纬区对地球轨道驱动全球气候的影响区分开来 ,才有可能正确预测未来气候的演变方向。  相似文献   

陕西及我国东部区域气候变化研究   总被引：6，自引：2，他引：4  

王川  杜继稳  杜川利  袁君健 《气象》2005,31(4):22-26

利用我国500多年旱涝资料,分析陕西及其东部区域历史上发生的旱涝周期及气候突变,发现陕西旱涝存在22年、169年左右的变化周期,陕西1645年左右发生过气候突变,分别比华北地区早6～7年,比华东地区早40～50年。同时分析近50年气候资料发现,陕西及东部地区降水均存在着一定的周期变化,且变化有所差异。定义了陕北区域旱涝指数,在未来十年,陕北地区旱涝变化趋势是正常偏旱。  相似文献   

基于Internet与GIS的全球禽流感时空动态分析   总被引：3，自引：0，他引：3  

孙根年  杨欢欢 《地理与地理信息科学》2006,22(6):24-29

全球禽流感的爆发具有年际尺度的周期性,且周期缩短、频率加快、危害增强,这种趋势与生态环境恶化有关;2003年以来全球禽流感的年内活动具有明显的季节性,多集中在秋末冬初和冬末春初,季节交替、气温变化剧烈是禽流感的诱发因素;通过对2000年以前和2003年以来禽流感发生地的制图研究,发现全球禽流感集中分布在从西欧、地中海、经西亚到东南亚再到拉丁美洲的弧形环带上,这里海陆交互作用强烈、飞禽和水禽活动集中,人类活动排放的某些化学毒物是病毒变异的诱因;将近年来全球禽流感时空分布与候鸟迁徙路线相比较,发现在亚欧非“世界岛”上的8条路线具有良好的对应关系,候鸟迁徙应是禽流感全球传播的重要途径。  相似文献   

全新世以来华北平原层圈间水循环演化过程与区域地下水演变周期性   总被引：6，自引：1，他引：6       下载免费PDF全文

张光辉  聂振龙  陈宗宇  赖勤波  王金哲 《地球学报》2001,22(4):293-297

该文阐述全新世以来大气圈，岩石圈，生物圈与水圈之间水文循环过程中水分通量的演化规律，揭示了近百年来人类活动对层圈之间水分通量变化的干扰作用，并依据全新世时期千年尺度和百所尺度水文循环演化的特点，分析和预测了华北平原区域地下水演变的周期性和未来30－50a趋势。  相似文献   

Analysis of meteorological drought variability in Niger and its connection with climate indices     

Zakari Seybou Abdourahamane  Reşat Acar 《水文科学杂志》2018,63(8):1203-1218

Based on a three-month-scale standardized precipitation index (SPI-3) computed from the available rainfall data of 13 stations of Niger, meteorological drought trends, periodicities and the relationships with 10 oceanic–atmospheric variables were analysed using the Mann-Kendall test, continuous wavelet transform and cross-wavelet analysis, respectively. The results revealed a significant (p < 5%) increase in drought at five of the 13 stations. A common dominant drought periodicity of 2 years was found at all of the stations, whereas significant periodicities varied from 2 to 32 years at six stations. Among the considered climate indices, South Atlantic sea-surface temperature, Southern Oscillation Index, sea-level pressure, geopotential height and relative humidity from the Atlantic basin oscillated in anti-phase relative to the SPI-3 at an inter-annual to decadal time scale from 1960 to 1990. In this period, relative humidity from the Mediterranean basin and zonal wind oscillated in phase with the drought index.  相似文献   

Erosion characteristics of loess tunnels on the Loess Plateau: A field investigation and experimental study     

Xi-An Li  Li Wang  Bo Hong  Lin-Cui Li  Jia Liu  Hao-nan Lei 《地球表面变化过程与地形》2020,45(9):1945-1958

Loess tunnels are a common geo-hazard in the Loess Plateau and not only cause considerable soil and water loss, but also aggravate and even induce the occurrence and development of other disasters such as ground fissures, mudflows, collapses, and landslides. To date, research on the hydrological characteristics and erosion behaviour of loess tunnel systems has focused on field investigation data and limited river basin observation data, whereas field test information and data are very scarce. In this study, field surveys, observations, field scouring experiments, and laboratory-based sediment percentage tests were conducted to analyse the erosion characteristics, spatial distribution, and hydrological characteristics of a large-scale loess tunnel system in the hilly Loess Plateau southeast region of northern China. The results showed that the loess tunnel erosion exhibited periodicity. Tunnel erosion in each period shows a similar erosion process, that is, thin-layer water flow erosion and lateral expansion, tunnel wall collapse and deposit due to the loss of support from the lateral erosion, and erosion and transport of deposits by water flow. Waterfall erosion, lateral erosion, headward erosion, and the resulting collapses were the main forms of tunnel erosion. Besides this, the base level of erosion significantly affects the erosion characteristics of the loess tunnel. The hydrological characteristics during field scouring experiments exhibited three different stages: a lag effect, attributed to the temporary loss of water velocity in the first stage; small water flow fluctuations in the second stage; and an increase in total seepage loss with increased water injection flow in the third stage. The erosion rate was positively correlated with the flow quantity. The results of this study not only provide valuable reference data for research on the mechanism and velocity of erosion events in loess, but also provide a theoretical basis for the prevention of loess tunnel disasters in engineering construction. © 2020 John Wiley & Sons, Ltd.  相似文献   

末次冰期以来南海南部千年尺度的古海洋学   总被引：1，自引：0，他引：1  

王良  刘传联 《海洋地质与第四纪地质》2008,28(4)

对南海南部MD05-2896柱状样22.8 kaBP以来的深海沉积物进行了浮游有孔虫和颗石藻化石定量分析.通过转换函数、特定有孔虫属种含量及比值和颗石藻Florisphaera profunda百分含量等探讨了南海南部海水表层温度、上部水体结构、初级生产力以及碳酸盐溶解作用等变化趋势和周期性.结果表明:18 kaBP以前及10 kaBP以来,海水表层温度较高,碳酸盐溶解作用较强,温跃层营养跃层较深,初级生产力较低.18～10 kaBP冰期时,海水表层温度最低,碳酸盐溶解作用变弱,营养跃层和温跃层变浅,初级生产力较高.频谱分析结果显示,22.8 kaBP以来的气候变化具有明显的周期性,以类D/O事件的千年尺度周期为主,其中最主要的周期为1 500年.  相似文献   

Mid‐ and late‐Holocene climatic changes: a test of periodicity and solar forcing in proxy‐climate data from blanket peat bogs     

Frank M. Chambers  Jeffrey J. Blackford 《第四纪科学杂志》2001,16(4):329-338

A wide range of palaeoenvironmental evidence from the Holocene has suggested periodicities in the Earth's climate of 10s to 1000s of years. Identifying these millennial‐, century‐ and decadal periodicities, and their impacts, is critical in developing a fuller understanding of natural climate variability. Any solar‐induced climatic change needs to be distinguished from other causes of natural climate variability and from short‐term catastrophic events induced either by external or internal processes. Such events might themselves generate a periodicity, or in combination with other forcing factors they may contribute towards a periodicity (and so spuriously imply a universal and continuing periodicity in the climate record), or they may resonate with a solar‐induced periodicity. Here, evidence from peat records for periodicity in climate change over the mid to late Holocene is reviewed and this is followed by a test of the replicability of claimed periodicities using blanket peat data covering the past 2000 yr from four sites in the British Isles. Results suggest that the mires studied do go through phases of being responsive to periodic forcing factors, with ca. 200, ca. 80 and 60–50 yr wavelengths reflected in some data sets. However, the patterns shown are not consistent. This could be the result of local conditions at individual mires (human impact, sensitivity and vegetation succession) or of changes in the strength or nature of global forcing factors. Assessing a solar–mire link remains difficult because the century‐scale variations of the Sun show different intervals between solar minima, the durations of which are themselves unequal, and because the proxy‐climate data‐sets from peat profiles may themselves not be dated with sufficient precision and/or accuracy. Copyright © 2001 John Wiley & Sons, Ltd.  相似文献   

新沂地电场日变化特征及频谱分析   总被引：1，自引：1，他引：0  

张彩艳  李飞  张秀霞  杨冯威  纪加迎 《地震地磁观测与研究》2011,32(5):72-77

通过对新沂地电场平静时段资料与地磁场资料对比分析,结果显示:新沂地震台地电场变化和变化磁场密切相关,其中NS向的主体变化和地磁场H分量的变化准同步;EW向主体变化虽与地磁场H分量变化有相同之处,但其变化形态与其反向,且不尽相同.运用快速傅里叶变换进行频谱分析,发现:新沂地电场NS向和EW向与地磁场H分量的优势周期存在不...  相似文献