磁尾中交换不稳定性所产生偶极化锋面的动力学特性研究          下载免费PDF全文

吕浩宇  李芸  葛亚松 《地球物理学报》2018,61(2):403-410

本文利用考虑了Hall效应和有限Larmor半径（FLR）效应的磁流体数值模拟研究了在离子惯性长度/离子Larmor半径尺度内偶极化锋面的动力学特性.偶极化锋面由磁尾近地区域中由于热压尾向梯度和磁场曲率力不平衡所引起的交换不稳定性自洽产生.数值研究表明,偶极化锋面是切向间断,在相对该锋面结构静止的参考系中等离子体穿过偶极化锋面的法向速度为零.Hall效应主要影响与偶极化锋面的切平面相正交的电场,使得锋面切向电流增大,同时产生锋面结构不对称.研究表明离子在Larmor半径尺度产生的FLR效应可导致锋面结构的大尺度漂移运动.由FLR效应产生的离子磁化流速在偶极化锋面的日下点处指向昏向,锋面后区域的速度晨向分量增长,从而导致整个锋面结构向晨向漂移.  相似文献   

Controls on the mechanisms of fluid infiltration and front advection during regional metamorphism: a stable isotope and textural study of retrograde Dalradian rocks of the SW Scottish Highlands     

J. B. FEIN  C. M. GRAHAM  M. B. HOLNESS  A. E. FALLICK  A. D. L. SKELTON 《Journal of Metamorphic Geology》1994,12(3):249-260

Vein-controlled retrograde infiltration of H₂O-CO₂ fluids into Dalradian epidote amphibolite facies rocks of the SW Scottish Highlands under greenschist facies conditions resulted in alteration of calcite-rich marble bands to dolomite and spatially associated ¹⁸O enrichment of about 10%. on a scale of metres. Fluid inclusion data indicate that the retrograde fluid was an H₂O-salt mixture with a low CO₂ content, and that the temperature of the fluid was about 400d? C. Detailed petrographic and textural (backscattered electron imaging) studies at one garnet-grade locality show that advection of fluid into marbles proceeded by a calcite-calcite grain edge flow mechanism, while alteration of non-carbonate wall-rock is associated with veinlets and microcracks. Stable isotopic analysis of carbonates from marble bands provides evidence for advection of isotopic fronts through carbonate wall-rocks perpendicular to dolomite veins, and fluid fluxes in the range 2.4–28.6 m³/m² have been computed from measured advection distances. Coincidence of isotope and reaction fronts is considered to result from reaction-enhanced kinetics of isotope exchange at the reaction front. Front advection distances are related to the proportion of calcite to quartz in each marble band, with the largest advection distance occurring in nearly pure calcite matrix. This relationship indicates that fluid flow in carbonates is only possible along fluid-calcite-calcite grain edges. However, experimental constraints on dihedral angles in calcite-fluid systems require that pervasive infiltration occurred in response to calcite dissolution initiated at calcite-calcite grain junctions rather than to an open calcite pore geometry. The regional extent of the retrograde infiltration event has been documented from the high δ¹⁸O of dolomite-ankerite carbonates from veins and host-rocks over an area of least 50 × 50 km in the SW Scottish Highlands. Isotopically exotic ¹⁸O-rich retrograde fluids have moved rapidly upwards through the crust, inducing isotopic exchange and mineral reaction in wall-rocks only where lithology, pore geometry or mineral solubilities, pressure and temperature have been appropriate for pervasive infiltration to occur.  相似文献   

Interaction of a nonstationary ionization-shock front with an inhomogeneous interstellar medium     

K. V. Krasnobaev 《Astronomy Letters》2001,27(9):568-573

We consider the interaction of an ionization-shock front with isothermal waves in an H I region. Based on a two-front model in the linear approximation, we have detected a significant (approximately by an order of magnitude) periodic amplification of perturbations as they penetrate from the interstellar medium into an H II region. Numerical simulations have revealed that even when the shock-and ionization-front velocities differ and the relative density perturbations in the interstellar medium are ～10^?1, the variations in gas parameters near the ionization front are comparable to those observed at the boundaries of H II regions.  相似文献   

基于MSORQ-Tree的三维景观地图表示     

胡亚芳  刘荣 《北京测绘》2014,(6):9-11

针对WebGIS多尺寸三维景观地图数据处理问题,提出了一种高速数据索引结构MSORQ-Tree。根据该索引的算法,得出移动WebGIS景观图,将该索引和其他索引进行性能比较。结果显示,基于金字塔分割规则的区域,进行分割四叉树所获取的MSORQ-Tree高速索引可有效处理WebGIS中海量景观地图数据。  相似文献   

Reply to Comment on ‘Marine GIS: Identification of mesoscale oceanic thermal fronts’     

V. Valavanis  I. Katara  A. Palialexis 《International journal of geographical information science》2013,27(3):375-378

Geographic information service (GIService) has become popular in the last decade to develop applications for addressing global challenges. Performance is one of the most important criteria to help users select distributed online GIService for developing geospatial applications including natural hazards and emergency responses. However, performance accuracy is limited by the single-location-based evaluation mechanism while service performance is dynamic in space and time between end-users and services. We propose a spatiotemporal performance evaluation mechanism to improve the accuracy. Specially, a cloud and volunteer computing mechanism is proposed to collect performance information of globally distributed GIServices. A global spatiotemporal performance model is designed to integrate spatiotemporal dynamics for better performance evaluation for users from different regions at different times. This model is tested to support GIService selection in global spatial data infrastructures (SDIs). The experiment confirms that the proposed model provides more accurate evaluations for global users and better supports geospatial resource utilizations in SDIs than previous mechanisms. The methodology can be adopted to improve the services of other regional and global distributed operational systems.  相似文献   

中国海洋产业的结构与布局研究展望   总被引：3，自引：0，他引：3  

马仁锋  李加林  赵建吉  庄佩君 《地理研究》2013,32(5):902-914

海洋产业结构与布局是海洋经济地理学研究的核心领域与主体内容,国内相关文献日益丰富,但海洋产业结构与布局研究尚未形成完整体系。梳理现有文献发现:国内研究存在起步晚、发展缓慢,高层次研究成果少且增长慢,以区域实证研究为主、理论创新研究较少等问题,现有研究集中在6方面:①海洋产业结构与布局的内涵、规律及其与陆域布局差异探索;②沿海省份或大城市海洋产业结构的现状与问题、结构优化与主导产业选择、产业结构绩效评价、竞争力与趋势研究;③区域海洋产业布局模式及优化政策支撑体系研究;④海洋资源与环境的产业承载力评价及海洋功能区划研究;⑤海洋产业集群,尤其是港航集群的初步探索;⑥国外海洋产业发展态势、统计标准与区域海洋产业合作探索。本文初步总结了国内对海洋产业结构与布局研究文献的增长规律,并立足于海洋产业结构与布局研究趋势,指出未来应加强海洋产业结构与布局的前沿领域及理论体系探索,并为我国海洋经济示范区建设提供科学指导。  相似文献   

Bathyal polychaete assemblages in the region of the Subtropical Front,Chatham Rise,New Zealand     

P. K. Probert  C. J. Glasby  S. L. Grove  B. L. Paavo 《新西兰海洋与淡水研究杂志》2013,47(5):1121-1135

Abstract

Polychaetes were collected from eight sites across the Chatham Rise (New Zealand) in the region of the Subtropical Front from water depths of c. 2300 m to 350 m. A total of 169 putative species representing 36 families was identified. Spionidae, Paraonidae, Cirratulidae, Syllidae, and Orbiniidae accounted for 50% of all polychaete individuals. Multivariate analysis revealed that three sites at c. 350–453 m water depth on muddy sand (6–7% clay) shared similar faunal and environmental characteristics. Numerical dominants included Lumbrineris sp., P seudeurythoe minuta, Dipolydora cf. socialis, Aglaophamus verrilli, Prionospio lehlersi, Syllinae sp., Monticellina sp., and Cossura sp. Replicates from a single site at c. 750 m depth on the southern flank of the Rise produced a distinct assemblage dominated by Paradoneis, Naineris, Notomastus, Harmothoinae, Prionospio lehlersi, Levinsenia, Aricidea, Kebuita, Paraonella, and ?Leiochrus species. Replicates from greater depths north and south of the Rise presented a greater range of assemblage characteristics and environmental parameters including temperature, dissolved oxygen, median grain size, calcium carbonate (CaCO₃), and total organic matter content. Twenty‐eight taxa were found exclusively below 750 m depths including species of Ampharetinae, Chloeia, Pseudeurythoe, Capitellidae, and Cirratulidae. There was a significant difference in faunal composition between northern and southern flanks of the Rise within depth classes and also between sites at the same depth classes. Faunal density and species diversity appeared highest from the crest to 750 m depth on the southern side. Low species diversity at the deepest sites may be confounded by reduced density.  相似文献   

Foraminiferal evidence for a pre‐middle eocene age of the chatham rise,New Zealand     

James P. Kennett  Richard E. Casey 《新西兰海洋与淡水研究杂志》2013,47(1):20-28

Several sediment samples collected from the crest and slope of the Chatham Rise, and from the Chatham Islands, to the east of New Zealand, contain Globigerina linaperta‐Globorotalia increbescens foraminiferal faunas of upper Middle and middle Upper Eocene age. The foraminiferal faunas from the Chatham Islands, which include Rectuvigerina, Latibolivina, Dyocibicides, Discorbinella, Patellina, and Wadella, indicate shallow‐water palaeodepths, probably equivalent to the outer shelf (50–150 m). A faunal assemblage from near the crest of the rise is likewise indicative of shallow water, although distinct differences in the benthonic foraminiferal ifauna suggest slightly deeper‐water biofacies than the Eocene of the Chatham Islands. In contrast, a fauna of similar age from 1,100 m on the southern slope of the Chatham Rise contains a much deeper‐water benthonic foraminiferal assemblage including Osangularia, Vulvulina, Stilostomella, hispidocostate Uvigerina, and smooth‐shelled Bulimina, indicative of lower middle bathyal depths (1,500–2,500 m).

The nature and distribution of the assemblages, together with previous work by Norris (1964) and Cullen (1965), indicates that the Chatham Rise has been a significant structure since at least the Middle Eocene, with some uplift occurring since then.  相似文献   

Mesoscale Variability in the Summer Arctic Boundary Layer     

Michael Tjernström  Thorsten Mauritsen 《Boundary-Layer Meteorology》2009,130(3):383-406

Observations from the summer Arctic Ocean Experiment 2001 (AOE-2001) are analysed with a focus on the interactions between mesoscale and boundary-layer dynamics. Wavelet analyses of surface-pressure variations show daylong periods with different characteristics, some featuring episodes of pronounced high-frequency surface-pressure variability, here hypothesized to be caused by trapped gravity waves. These episodes are accompanied by enhanced boundary-layer turbulence and an enhanced spectral gap, but with only minor influence on the surface stress. During these episodes, mesoscale phenomena were often encountered and usually identified as front-like features in the boundary layer, with a peak in drizzle followed by changing temperature. These phenomena resemble synoptic fronts, though they are generally shallow, shorter-lasting, have no signs of frontal clouds, and do not imply a change in air mass. Based on this analysis, we hypothesize that the root cause of the episodes with high-frequency surface-pressure variance are shallow, mesoscale fronts moving across the pack ice. They may be formed due to local-to-regional horizontal contrasts, for example, between air with different lifetimes over the Arctic or with perturbations in the cloud field causing differential cooling of the boundary layer. Thermal contrasts sharpen as the air is transported with the mean flow. The propagating mesoscale fronts excite gravity waves, which affect the boundary-layer turbulence and also seem to favour entrainment of free tropospheric air into the boundary layer.  相似文献   

Steering of upper ocean currents and fronts by the topographically constrained abyssal circulation     

Harley E. Hurlburt  E. Joseph Metzger  Patrick J. Hogan  Charles E. Tilburg  Jay F. Shriver   《Dynamics of Atmospheres and Oceans》2008,45(3-4):102

A two-layer theory is used to investigate (1) the steering of upper ocean current pathways by topographically constrained abyssal currents that do not impinge on the bottom topography and (2) its application to upper ocean – topographic coupling via flow instabilities where topographically constrained eddy-driven deep mean flows in turn steer the mean pathways of upper ocean currents and associated fronts. In earlier studies the two-layer theory was applied to ocean models with low vertical resolution (2–6 layers). Here we investigate its relevance to complex ocean general circulation models (OGCMs) with high vertical resolution that are designed to simulate a wide range of ocean processes. The theory can be easily applied to models ranging from idealized to complex OGCMs, provided it is valid for the application. It can also be used in understanding some persistent features seen in observed ocean frontal pathways (over deep water) derived from satellite imagery and other data. To facilitate its application, a more thorough explanation of the theory is presented that emphasizes its range of validity. Three regions of the world ocean are used to investigate its application to eddy-resolving ocean models with high vertical resolution, including one where an assumption of the two-layer theory is violated. Results from the OGCMs with high vertical resolution are compared to those from models with low vertical resolution and to observations. In the Kuroshio region upper ocean – topographic coupling via flow instabilities and a modest seamount complex are used to explain the observed northward mean meander east of Japan where the Kuroshio separates from the coast. The Japan/East Sea (JES) is used to demonstrate the impact of upper ocean – topographic coupling in a relatively weak flow regime. East of South Island, New Zealand, the Southland Current is an observed western boundary current that flows in a direction counter to the demands of Sverdrup flow and counter to the direction simulated in nonlinear global flat bottom and reduced gravity models. A model with high vertical resolution (and topography extending through any number of layers) and a model with low vertical resolution (and vertically compressed but otherwise realistic topography confined to the lowest layer) both simulate a Southland Current in the observed direction with dynamics depending on the configuration of the regional seafloor. However, the dynamics of these simulations are very different because the Campbell Plateau and Chatham Rise east and southeast of New Zealand are rare features of the world ocean where the topography intrudes into the stratified water column over a relatively broad area but lies deeper than the nominal 200 m depth of the continental shelf break, violating a limitation of the two-layer theory. Observations confirm the results from the high vertical resolution model. Overall, the model simulations show increasingly widespread upper ocean – topographic coupling via flow instabilities as the horizontal resolution of the ocean models is increased, but fine resolution of mesoscale variability and the associated flow instabilities are required to obtain sufficient coupling. As a result, this type of coupling is critical in distinguishing between eddy-resolving and eddy-permitting ocean models in regions where it occurs.  相似文献