耦合PMF、CMB模型对大气颗粒物源解析的研究     

刘莉  邹长武 《成都信息工程学院学报》2013,(5):557-562

化学质量平衡法是目前应用最为广泛的大气颗粒物源解析受体模型之一。针对利用化学质量平衡法进行源解析时,需建立大量的污染源成分谱,耗财耗力,同时选择不同的污染源及特征元素拟合时易导致源解析结果不确定性的问题,结合正矩阵因子分解法模型,提出了化学质量平衡法与正矩阵因子分解法的耦合模型,利用正矩阵因子分解法模型解析出各污染源及其特征元素,确定化学质量平衡法模型拟合参数及污染源清单。对比各污染源的理论贡献量与模拟贡献量,结果表明,耦合模型拟合结果与理论值差异不大,验证了耦合模型的可行性。耦合模型缩减了化学质量平衡法模型建立污染源成分谱的工作量,提高了化学质量平衡法模型进行源解析工作的高效性、准确性。  相似文献   

基于高斯平滑滤波的罗兰C周期识别新方法     

吴苗  李方能  苏晓庆  王国成 《海洋测绘》2013,(6):80-82

在有效估计天波延迟地波时间的基础上,提出了全新的基于高斯平滑滤波的罗兰C周期识别新方法。该方法完全摆脱了固定第三周期识别的思路,在有效防止信号出现周跳和确保接收机接收性能的精确性与稳定性的同时,提高了采样信号的信噪比,降低了信号电平的损失,增加了信息的利用率。  相似文献   

Numerical simulation of the effect of lower positive charge region in thunderstorms on different types of lightning   总被引：2，自引：0，他引：2  

YongBo Tan  ZhongWu Liang  Zheng Shi  JunRu Zhu  XiuFeng Guo 《中国科学:地球科学(英文版)》2014,57(9):2125-2134

Combined with the existing stochastic lightning parameterization scheme, a classic tripole charge structure in thunderstorms is assumed in the paper, and then 2-dimensional fine-resolution lighting discharge simulations are performed to quantitatively investigate the effect of lower positive charge (LPC) on different types of lightning. The results show: (1) The LPC plays a key role in generating negative cloud-to-ground (CG) flashes and inverted intra-cloud (IC) lightning, and with the increase of charge density or distribution range of LPC region, lightning type changes from positive polarity IC lightning to negative CG flashes and then to inverted IC lightning. (2) Relative to distribution range of charge regions, the magnitude of charge density of the LPC region plays a dominant role in lightning type. Only when the maximal charge density value of LPC region is within a certain range, can negative CG flashes occur, and the occurrence probability is relatively fixed. (3) In this range, the charge density and distribution range of LPC region jointly determine the occurrence of negative CG flashes, which has a linear boundary with the trigger condition of IC lightning. (4) The common effect of charge density and distribution range of the LPC region is to change the distribution of positive potential well of bottom part of thunderstorms, and inverted IC lightning occurs when the initial reference potential is close to 0 MV, and negative CG flashes occur when the initial reference potential is far less than 0 MV.  相似文献   

The Evolution of a Meso-β-Scale Convective Vortex in the Dabie Mountain Area   总被引：1，自引：0，他引：1       下载免费PDF全文

XU Wenhui  NI Yunqi  WANG Xiaokang  QIU Xuexing 《Acta Meteorologica Sinica》2012,26(5):597-613

The evolution of a mesoscale convective system (MCS) that caused strong precipitation in the northern area of Dabie Mountain during 21-22 June 2008 is analyzed, along with the evolution of the associated meso-β-scale convective vortex (MCV). The mesoscale reanalysis data generated by the Local Analysis and Prediction System (LAPS) at a 3-km horizontal resolution and a 1-h time resolution during the South China Heavy Rainfall Experiment (SCHeREX) were utilized. The results show that two processes played key roles in the enhancement of convective instability. First, the mesoscale low-level jet strengthened and shifted eastward, leading to the convergence of warm-wet airflow and increasing convective instability at middle and low levels. Second, the warm-wet airflow interacted with the cold airflow from the north, causing increased vertical vorticity in the vicinity of steeply sloping moist isentropic surfaces. The combined action of these two processes caused the MCS to shift progressively eastward. Condensation associated with the MCS released latent heat and formed a layer of large diabatic heating in the middle troposphere, increasing the potential vorticity below this layer. This increase in potential vorticity created favorable conditions for the development of a low-level vortex circulation. The vertical motion associated with this low-level vortex further promoted the development of convection, creating a positive feedback between the deep convection and the low-level vortex circulation. This feedback mechanism not only promoted the maturation of the MCS, but also played the primary role in the evolution of the MCV. The MCV formed and developed due to the enhancement of the positive feedback that accompanied the coming together of the center of the vortex and the center of the convection. The positive feedback peaked and the MCV matured when these two centers converged. The positive feedback weakened and the MCV began to decay as the two centers separated and diverged.  相似文献   

一类偶数阶Sturm-Liouvile四点边值问题多个正解的存在性     

沈志默  肖建中  曹银芳 《南京气象学院学报》2012,4(1):92-96

讨论了一类偶数阶四点边值问题正解的存在性,借助Leggett-Williams不动点定理和不等式技巧,得到了该边值问题至少存在三个和任意奇数个正解的充分条件.  相似文献   

龙门山前陆褶皱冲断带的平衡剖面分析   总被引：49，自引：10，他引：39  

陈竹新  贾东  张惬  魏国齐  李本亮  魏东涛  沈扬 《地质学报》2005,79(1):38-45

对龙门山前陆褶皱冲断带形成的正反转构造过程有过许多分析 ,但明显缺乏直接的证据和定量的分析。本文在地层资料分析的基础上 ,借助平衡剖面分析验证龙门山形成的正反转构造过程 :志留纪至中三叠世受多条倾向北西的同沉积断裂控制 ;晚三叠世以来遭受北西—南东向挤压、抬升和剥蚀 ,形成逆冲推覆构造。在晚三叠世和新生代的两期板块碰撞的影响下 ,龙门山产生了两期褶皱冲断作用 ,但在南、北两段表现出显著不同的变形过程。龙门山北段表现为复杂的逆冲推覆构造 ,能明确划分出两期构造变形 ,晚三叠世的变形强烈 ,缩短率达 31.7% ;而新生代的变形较弱 ,缩短率仅为 10 .5 %。南段则表现出基底卷入的叠瓦状冲断的特点 ,主要体现新生代的构造变形 ,晚三叠世的构造变形基本上被改造 ,南段整体缩短率达 2 6 .2 %。  相似文献   

科其喀尔冰川表碛区冰崖消融的度日因子研究   总被引：1，自引：1，他引：0  

韩海东  王建  王欣  张鹏飞 《冰川冻土》2009,31(4):620-627

度日因子.冰崖坡向的变化也对度日因子产生了影响,总体表现为NEE-SE方向及SW-W方向的度日因子较大,NWW-N-NE方向的较小,S方向的最小,这主要与该地区的辐射、气温等气象条件的变化特征有关.研究还表明,冰崖的坡度对度日因子的影响较小.  相似文献   

液动锤套管起拔器的研制与应用          下载免费PDF全文

孙天  苗晓晓  叶兰肃  刘建福  王建兴  孙秀梅  刘莎莎  王越光 《探矿工程》2017,44(6):6-12

液动锤套管起拔器的原理是利用冲洗液作为动力介质,推动冲击锤产生振动,将机械应力波通过液动锤传至套管,使其松动后拔起。新研制的液动锤套管起拔器减轻了普通蛮力起拔方法对套管的损伤,节约钻探成本。本文介绍了双作用和正作用两种液动锤套管起拔器的起拔原理以及工作方法,并介绍了其在河北省遵化市西山带铁矿区进行野外试验中取得的效果。  相似文献   

可压缩层流边界层系统的一些性质     

杜翠  罗圆 《成都信息工程学院学报》2010,(6):324-327

进一步研究了可压缩流边界层系统解的一些性质,给出了可压缩边界层系统等价的奇异积分方程解存在时参数所在的区间,并通过研究等价的奇异积分方程解的性质,得出可压缩层流边界层系统给出剪应力函数厂和温度函数g的一些结果．  相似文献   

Positive and negative terrains on northern Shaanxi Loess Plateau     

ZHOU Yi  TANG Guo'an  YANG Xin  XIAO Chenchao  ZHANG Yuan  LUO Mingliang 《地理学报》2010,20(1):64-76

The Loess positive and negative terrains (P–N terrains), which are widely distributed on the Loess Plateau, are discussed for the first time by introducing its characteristic, demarcation as well as extraction method from high-resolution Digital Elevation Models. Using 5 m-resolution DEMs as original test data, P–N terrains of 48 geomorphological units in different parts of Shaanxi Loess Plateau are extracted accurately. Then six indicators for depicting the geomorphologic landscape and spatial configuration characteristic of P–N terrains are proposed. The spatial distribution rules of these indicators and the relationship between the P–N terrains and Loess relief are discussed for further understanding of Loess landforms. Finally, with the integration of P–N terrains and traditional terrain indices, a series of un-supervised classification methods are applied to make a proper landform classification in northern Shaanxi. Results show that P–N terrains are an effect clue to reveal energy and substance distribution rules on the Loess Plateau. A continuous change of P–N terrains from south to north in Shaanxi Loess Plateau shows an obvious spatial difference of Loess landforms and the positive terrain area only accounted for 60.5% in this region. The P–N terrains participant landform classification method increases validity of the result, especially in the Loess tableland, Loess tableland-ridge and the Loess low-hill area. This research is significant on the study of Loess landforms with the Digital Terrains Analysis methods.  相似文献