基于小波变换的大安地区年降水量变化特征   总被引：3，自引：0，他引：3  

卢文喜  陈社明  王晨子  刘磊  贾洪玮  吕德全 《吉林大学学报(地球科学版)》2010,40(1):121-127

基于小波分析的方法,对吉林省大安地区1959—2007年的年降水量序列的变化特征进行了分析。经分析表明,大安地区年降水量在其计算时域内各时间尺度分布不均匀,具有明显的局部化特征;其中4～6 a尺度主要发生在1959—1969年和1984年之后,10～12 a尺度主要发生在1965—1999年,20～25a尺度在整个计算时域内均有发生。不同时间尺度下,降水量偏多、偏少交替变化也不相同。此外,分析结果显示该地区年降水量具有4 a、10 a和21 a左右的主周期,其中4 a周期为第一主周期。  相似文献   

影响副高活动的热力强迫作用——动力学解析模型   总被引：2，自引：1，他引：1  

张韧  董兆俊  洪梅 《气象科学》2010,30(5):646-649

采用最优化搜索方法,对影响副高活动的东亚季风区位势场和季风雨带降水场进行了函数拟合,并用拟合出的函数作为基函数和热力强迫因子代入正压涡度方程,对涡度方程解的性质进行了讨论。分析和模拟结果表明:中心位于我国华北一带东亚季风雨带凝结潜热释放易导致副高的西伸和北抬;而中心位于赤道附近的南海季风槽降水热力作用可导致副高出现东退和西伸两种可能。  相似文献   

Towards an understanding of the Of?p star HD 191612: optical spectroscopy   总被引：1，自引：0，他引：1  

Ian D. Howarth  Nolan R. Walborn  Danny J. Lennon  Joachim Puls  Yaël Nazé  K. Annuk  I. Antokhin  D. Bohlender  H. Bond  J.-F. Donati  L. Georgiev  D. Gies  D. Harmer  A. Herrero  I. Kolka  D. McDavid  T. Morel  I. Negueruela  G. Rauw  P. Reig 《Monthly notices of the Royal Astronomical Society》2007,381(2):433-446

We present extensive optical spectroscopy of the early-type magnetic star HD 191612 (O6.5f?pe–O8fp). The Balmer and He  i lines show strongly variable emission which is highly reproducible on a well-determined 538-d period. He  ii absorptions and metal lines (including many selective emission lines but excluding He  ii λ4686 Å emission) are essentially constant in line strength, but are variable in velocity, establishing a double-lined binary orbit with   P _orb= 1542 d, e = 0.45  . We conduct a model-atmosphere analysis of the spectrum, and find that the system is consistent with a ∼O8 giant with a ∼B1 main-sequence secondary. Since the periodic 538-d changes are unrelated to orbital motion, rotational modulation of a magnetically constrained plasma is strongly favoured as the most likely underlying 'clock'. An upper limit on the equatorial rotation is consistent with this hypothesis, but is too weak to provide a strong constraint.  相似文献   

Toward 2050: the past is not the key to the future – challenges for the science of geochemistry     

W. S. Fyfe 《Environmental Geology》1998,33(2-3):92-95

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Stochastic micromechanical model of the deterioration of asphalt mixtures subject to moisture diffusion processes     

Silvia Caro  Eyad Masad  Mauricio Sánchez‐Silva  Dallas Little 《国际地质力学数值与分析法杂志》2011,35(10):1079-1097

The deleterious effect of moisture in the microstructure of asphalt mixtures, usually referred to as moisture damage, has been recognized as a main cause of early deterioration of asphalt pavements. The initiation and evolution of moisture‐related deterioration is strongly influenced by the internal air void structure of asphalt mixtures. Despite its importance, the majority of works conducted on the micromechanical modeling of asphalt mixtures overlook the role of the air void structure, mainly because of its high complexity and variability. This paper explores the influence of air void variability on the performance of asphalt mixtures subjected to moisture diffusion processes. A stochastic modeling technique based on random field theory was used to generate internal distributions of physical and mechanical properties of the asphalt matrix of the mixture that depend on probable air voids distributions. The analysis was conducted by means of a coupled numerical micromechanical model of moisture damage. The results showed that the variability and distribution of air voids are decisive in determining the moisture‐dependent performance of asphalt mixtures. Furthermore, it was also shown that a stochastic characterization of the diverse air void configurations is a feasible and useful approach to better represent and understand mechanically related deterioration processes in asphalt mixtures. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

Latitude-Dependent Response of East Asian Summer Monsoon to External Forcing in the Last Millennium     

GU Yajin  WANG Hongli  LIU Jian 《Acta Meteorologica Sinica》2010,24(6):671-679

Response of the East Asian summer monsoon(EASM) rainfall to external forcing(insolation,volcanic aerosol,and greenhouse gases) is investigated by analysis of a millennium simulation with the coupled climate model ECHO-G.The model reproduces reasonably realistic present-day EASM climatology.The simulated precipitation variation in East Asia over the last millennium compares favorably with the observed and proxy data.It is found that the features and sensitivity of the forced response depend on latitude.On...  相似文献   

海洋测深综合效应的多测线改正技术     

于家城  宋春雷  徐学强  陈家斌 《海洋测绘》2008,28(2):9-12

提出了水深测量综合效应的多测线改正技术，通过分析水深测量中的波束角效应、地势效应及载体姿态变化对测深的影响，给出二维数字测深仪的详细设计方法，建立描述水深改正的指标，并用实际地形进行仿真。结果标明，该方法实用性强、改正效果明显。  相似文献   

Accretion to stars with non-dipole magnetic fields   总被引：1，自引：0，他引：1  

M. Long  M. M. Romanova  R. V. E. Lovelace 《Monthly notices of the Royal Astronomical Society》2007,374(2):436-444

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Three-dimensional simulations of molecular cloud fragmentation regulated by magnetic fields and ambipolar diffusion     

Takahiro Kudoh  Shantanu Basu  Youichi Ogata  Takashi Yabe 《Monthly notices of the Royal Astronomical Society》2007,380(2):499-505

We employ the first fully three-dimensional simulation to study the role of magnetic fields and ion–neutral friction in regulating gravitationally driven fragmentation of molecular clouds. The cores in an initially subcritical cloud develop gradually over an ambipolar diffusion time while the cores in an initially supercritical cloud develop in a dynamical time. The infalling speeds on to cores are subsonic in the case of an initially subcritical cloud, while an extended (≳0.1 pc) region of supersonic infall exists in the case of an initially supercritical cloud. These results are consistent with previous two-dimensional simulations. We also found that a snapshot of the relation between density (ρ) and the strength of the magnetic field ( B ) at different spatial points of the cloud coincides with the evolutionary track of an individual core. When the density becomes large, both the relations tend to   B ∝ρ^0.5  .  相似文献   

胜利油田火山岩类、盆地演化及其CO₂-Au成藏成矿效应   总被引：15，自引：5，他引：15       下载免费PDF全文

赫英  王定一  廖永胜 《地质科学》2001,36(4):454-464

将胜利油田盆地内火山岩类分为石英拉斑玄武岩、橄榄拉斑玄武岩和碱性橄榄玄武岩3类。其中,碱性橄榄玄武岩多分布于盆地边部、出现较晚并受深断裂控制,其成分中明显更富碱、富轻稀土、富大离子亲石元素而贫铬、镍等相容元素和挥发分,深度大而熔融程度不高,应源于富集地幔。二氧化碳气藏与碱性橄榄玄武岩有空间、时间和成因上的关系;二氧化碳气藏区的火山岩中含有高含量的金。二氧化碳和金是盆地和火山岩类演化一定阶段的产物,源于富集地幔的岩浆去气是其形成的主要机制。  相似文献