On the coalescence of twisted flux tubes     

Arnab Rai Choudhuri 《地球物理与天体物理流体动力学》2013,107(3-4):261-291

Abstract

We study the problem of the coalescence of twisted flux tubes by assuming that the azimuthal field lines reconnect at a current sheet during the coalescence process and everywhere else the magnetic field is frozen in the fluid. We derive relations connecting the topology of the coalesced flux tube with the topologies of the initial flux tubes, and then obtain a structure equation for calculating the field configuration of the coalesced flux tube from the given topology. Some solutions for the two extreme cases of low-β plasma and high-β plasma are discussed. The coalesced flux tube has less twist than the initial flux tube. Magnetic helicity is found to be exactly conserved during the coalescence, but the assumptions in the model put a constraint on the energy dissipation so that we do not get a relaxation to the minimum-energy Taylor state in the low-β case. It is pointed out that the structure equation connecting the topology and the equilibrium configuration is quite general and can be of use in many two-dimensional flux tube problems.  相似文献   

A mesoscopic model for the behaviour of concrete under high confinement     

F. Dupray  Y. Malecot  L. Daudeville  E. Buzaud 《国际地质力学数值与分析法杂志》2009,33(11):1407-1423

When impact loaded, concrete is submitted to high triaxial stresses. The experimental response of concrete under quasi‐static triaxial compression is studied using a triaxial press capable of applying a mean pressure greater than 1 GPa on cylindrical samples measuring 7 cm in diameter and 14 cm high. A numerical analysis of these previous experiments is performed herein at a mesoscopic scale. Concrete is modelled as a biphasic material consisting of a mortar (cement paste and fine aggregates) and roughly spherical aggregates (with a diameter exceeding 2 mm) whose characteristics are applied on a regular cubic finite element mesh. A damage‐plasticity model is then used to model the behaviour of mortar. An identification of model parameters on mortar samples and the subsequent comparison between numerical and experimental tests will be presented for hydrostatic and triaxial compression. Copyright © 2009 John Wiley & Sons, Ltd.  相似文献   

梅雨锋暴雨雨团运动场结构演变模拟分析     

贺哲  李平  康雯瑛 《气象》2005,31(6):19-23

利用中尺度数值模式MM5对1998年7月29-30日发生于长江中下游的暴雨过程进行了模拟。对两个相邻雨团的运动场结构进行分析，揭示了梅雨锋暴雨雨团的相互作用对其运动场结构的影响。分析表明，由于新雨团的生成，原有邻近雨团上升气流结构由一种形式的不对称转为另一种形式的不对称。中尺度涡管不仅在垂直方向呈波状，在水平方向也随着雨团位置和降雨的强弱而波动。  相似文献   

一次弱对流引发局地特大暴雨天气的诊断分析   总被引：4，自引：1，他引：4  

刘勇  王川 《气象》2005,31(8):14-18

对2003年8月28-29日宁陕特大暴雨过程诊断分析结果表明：特大暴雨发生在低层辐合、高层辐合，不利于强对流发展的弱对流环境中。低层850～700hPa低涡倒槽为特大暴雨提供了辐合上升运动和充沛的水汽条件。850hPa几股来自不同方向、性质不同的气流相汇在宁陕上空，强水汽辐合是特大暴雨形成的主要原因。  相似文献   

“04.6”湘西北特大致洪暴雨形成机理分析   总被引：8，自引：0，他引：8  

刘志雄  戴泽军  叶成志  李耨周  陈勇 《气象》2005,31(10):61-67

对湖南省西部和北部的一次特大致洪暴雨过程综合分析得出：此次特大暴雨过程的发生与对流层中低层西南急流和亚欧大陆上空维持阻塞形势密切相关。阻塞形势的维持，使得对流层中低层两个冷涡稳定少动，从而形成了东北向干冷气流，其与西南暖湿气流在湘西北地区上空形成一条东北西南向的切变线。切变线上生成的深厚的中尺度气旋的演变、发展，是特大暴雨产生的根本原因。对流层中层涡度、Q矢量散度及345K等熵面上位势涡度的由南向北发展与强降水区由南向北发展有较好的对应关系，可作为暴雨预报指标。超强散度柱、强涡度柱和陡立深厚θse，耦合结构是垂直上升动力和暴雨产生和持续的重要动力机制。  相似文献   

“2004.7”沙澧河流域特大暴雨成因分析     

胡燕平  肖刚  惠付梅  王颖  白红霞  董羽仑  程锦霞 《气象》2005,31(12):32-35

应用常规、加密气象资料及卫星云图,分析了2004年7月16～17日沙澧河流域特大暴雨成因.结果表明：高、低空急流耦合区中西南低涡及MCC特征云团的形成和维持是造成此次特大暴雨的直接影响系统.提出利用逐时的中尺度辐合中心、卫星红外云图云顶亮温及雷达回波降水率做中尺度雨团量级预测思路.  相似文献   

一次低纬高原特大暴雨天气的诊断分析   总被引：4，自引：1，他引：4  

李宏波  何萍 《气象》2005,31(3):77-80

结合大尺度环流的高通滤波、卫星云图和雷达回波诊断，通过地面天气图分析等方法，对2003年6月17日云南中部的楚雄市至南华县一带发生的特大暴雨过程进行了中尺度分析。结果表明，这次过程是热带中尺度气旋东南移并发展造成的；地面强冷空气侵入中尺度低压导致对流发展，是热带中尺度气旋加强的原因；大尺度环流下，孟加拉湾、南海和北部湾形成的两条水汽输送带通过热带低压为强对流的发展和维持提供了能源保障；地面中尺度低压中心和与之配置的切变线北侧对特大暴雨落区有较好的指示。  相似文献   

南宁雷达责任区强对流天气的气候统计特征分析   总被引：2，自引：0，他引：2  

陈阳  陆春菊 《广西气象》2005,26(2):16-17

对1958～2002年共计44a内，前汛期（2～6月）南宁雷达责任区内的冰雹、短时大风等强对流天气进行了气候统计分析，以及分析了强对流天气对应的影响天气系统，得到了一些有价值的气候时空分布特征规律。  相似文献   

2002年12月下旬宁夏持续低温天气成因分析          下载免费PDF全文

陈楠 《山西气象》2005,(2):23-26

本文主要通过发生在山西境内的一次强对流天气过程,简单介绍2003年3月份移植的敏视达气象应用软件包在强对流天气方面的应用。  相似文献   

An Analysis of a Meso-β System in a Mei-yu Front Using the Intensive Observation Data During CHeRES 2002   总被引：3，自引：0，他引：3  

SUN Jianhu  ZHANG Xiaoling  QI Linlin  ZHAO Sixiong 《大气科学进展》2005,22(2):278-289

The conventional and intensive observational data of the China Heavy Rain Experiment and Study (CHeRES) are used to specially analyze the heavy rainfall process in the mei-yu front that occurred during 20-21 June 2002, focusing on the meso-β system. A mesoscale convective system (MCS) formed in the warm-moist southwesterly to the south of the shear line over the Dabie Mountains and over the gorge between the Dabie and Jiuhua Mountains. The mei-yu front and shear line provide a favorable synoptic condition for the development of convection. The GPS observation indicates that the precipitable water increased obviously about 2-3h earlier than the occurrence of rainfall and decreased after that. The abundant moisture transportation by southwesterly wind was favorable to the maintenance of convective instability and the accumulation of convective available potential energy (CAPE). Radar detection reveals that meso-β and -γ systems were very active in the MαCS. Several convection lines developed during the evolution of the MαCS, and these are associated with surface convergence lines. The boundary outflow of the convection line may have triggered another convection line. The convection line moved with the mesoscale surface convergence line, but the convective cells embedded in the convergence line propagated along the line. On the basis of the analyses of the intensive observation data, a multi-scale conceptual model of heavy rainfall in the mei-yu front for this particular case is proposed.  相似文献