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51.
台风Mindulle变性再发展的特征及机理研究 总被引:1,自引:0,他引:1
对于2004年台风Mindulle登陆入海再发展进行研究分析。通过演变特征的分析,发现在台风北移时,冷空气入侵台风低层,台风经历一个变性再发展的过程,台风在高层一直保持暖心结构,并且在台风的西侧形成一个冷锋面结构,而在北侧为一个暖性锋面结构,使得暖空气被迫抬升,冷空气也逐渐包围了台风。冷平流与来自暖海面的暖平流交汇使得暖湿的海面对流加剧。同时高空急流入口处辐散区与台风低压的重合和西风槽的东移,对台风的维持和再发展起到了重要的作用。 相似文献
52.
Hadi Alkahby 《地球物理与天体物理流体动力学》2013,107(4):335-346
In this article, we examine reflection, dissipation and attenuation of vertically propagating waves in an isothermal atmosphere under the combined effect of Newtonian cooling, thermal conduction and viscosity with a weak horizontal magnetic field. We consider the case in which the combined effect of viscosity and magnetic field is dominated by that of the thermal conduction and for small values of the Newtonian parameter. As a result, the atmosphere can be divided into three distinct regions that are connected by two transition regions. The lower and middle regions are connected by a semi-transparent barrier and the middle and upper regions are connected by an absorbing and reflecting barrier. In the connecting barriers the reflection and transmission of the waves takes place. The presence of Newtonian cooling effects on the adiabatic region, produces attenuation in the amplitudes of the waves and reduces the energy absorption in the transition regions. The reflection coefficient is determined in the lower and middle regions and the results are discussed in the context of the heating of the solar atmosphere. 相似文献
53.
Strength and deformation behavior of the Shimanto accretionary complex across the Nobeoka thrust 下载免费PDF全文
A rapid reduction in sediment porosity from 60 to 70 % at seafloor to less than 10 % at several kilometers depth can play an important role in deformation and seismicity in the shallow portion of subduction zones. We conducted deformation experiments on rocks from an ancient accretionary complex, the Shimanto Belt, across the Nobeoka Thrust to understand the deformation behaviors of rocks along plate boundary faults at seismogenic depth. Our experimental results for phyllites in the hanging wall and shale‐tuff mélanges in the footwall of the Nobeoka Thrust indicate that the Shimanto Belt rocks fail brittlely accompanied by a stress drop at effective pressures < 80 MPa, whereas they exhibit strain hardening at higher effective pressures. The transition from brittle to ductile behavior in the shale–tuff mélanges lies on the same trend in effective stress–porosity space as that for clay‐rich and tuffaceous sediments subducting into the modern Nankai subduction zone. Both the absolute yield strength and the effective pressure at the brittle–ductile transition for the phyllosilicate‐rich materials are much lower than for sandstones. These results suggest that as the clay‐rich or tuffaceous sediments subduct and their porosities are reduced, their deformation behavior gradually transitions from ductile to brittle and their yield strength increases. Our results also suggest that samples of the ancient Shimanto accretionary prism can serve as an analog for underthrust rocks at seismogenic depth in the modern Nankai Trough. 相似文献
54.
Renewed attention to the role of subnational efforts in addressing myriad environmental challenges necessitates a greater understanding of the factors associated with program adoption. Given observed relationships between adoption of sustainability practices and the presence of carbon-intensive industry, and separately the observed persistence of industrial history in a given place, we explore the link between historical manufacturing employment volatility and current sustainability plan adoption at the local level. Our analysis suggests that the magnitude of changes in manufacturing employment is inversely related to the likelihood of sustainability plan adoption. Our analysis further suggests that, given the same pace of change, counties with shrinking manufacturing employment are more likely to adopt sustainability plans than those with growing employment. Lastly, we find that the link between past industrial transitions and local sustainability commitment is moderated by local disaster experience and priority for environmental protection. Collectively, the findings also shed light on potential—and otherwise unobservable—barriers to transitions to sustainable practices at the local level. In particular, the inverse relationship between pace of employment change and plan adoption suggests that minimizing the rapidity of contemporary transitions may counterintuitively ease the eventual adoption of sustainability-related policies. 相似文献
55.
夏季季风转换期间南沙群岛海域的温盐分布特征 总被引:2,自引:0,他引:2
应用2002年5月9-22日南沙群岛海域的水文观测资料,分析了季风转换期间南沙群岛海域的水文状况,并对比了调查海域不同区域的温盐分布特征。结果表明,夏季风转换期间海洋表层温度较高,基本在30℃以上,垂直结构上温度层结比较稳定。东北一西南走向界线两侧海域的温盐状况有明显的差异:西北部海域温度较高,垂向上有逆盐层现象;东南部海域温度相对较低,盐度的垂向结构上显示有双跃层现象,两海区水文特征的差异与季风结构和局地环流有密切的关系。从连续站温盐的时空剖面图可以看到,跃层以下,不规则的半日周期内潮对温盐分布有显著的影响。 相似文献
56.
我国主要育珠贝(蚌)贝壳珍珠层的扫描电子显微镜研究 总被引:8,自引:0,他引:8
采用扫描电子显微镜(SEM)对我国海水马氏珍珠贝Pinctada martensi(Dunker),大珠母贝Pinctada maxima(Jameson)、企鹅珍珠贝Pteria penguin(Roeding)和淡水三角帆蚌Hy-riopsis cumingii(Lea)贝壳珍珠层内层面的形貌特征进行了研究,结果表明,4种贝壳珍珠层均呈砖墙式结构,珍珠层中文五笔型小板片呈不规则多边形至六边形,直径为1.3-4.5μm,厚度0.35-0.85μm,同一种类贝壳中文石小板片的形状及粒径均匀一致,反映了生物矿物化的特殊性。珍珠层沿壳内层面与棱柱层过滤带中均存在初始生长的文石小晶体结构排列较混乱的现象,与成熟珍珠层中文石小板片的定向排列结构明显不同。 相似文献
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59.
Hugo Moreira Luís Seixas Craig Storey Mike Fowler Stephanie Lasalle Ross Stevenson Cristiano Lana 《地学前缘(英文版)》2018,9(4):977-995
Plutonic rocks from the Mineiro Belt, Brazil record a delayed onset of the transition from TTG to sanukitoid-type magmatism(high Ba-Sr), starting during the Siderian magmatic lull when little juvenile magma was added to the continental crust. Rocks mostly belong to the calc-alkaline series, meta-to peraluminous and originally "Ⅰ-type",meaning that oxidized magmas were formed by partial melting of subducted material. The temporal distribution and apparent secular changes of the magmas are consistent with the onset of subduction-driven plate tectonics due to an increase of the subduction angle and opening of the mantle wedge. New isotopic analyses(Sm-Nd whole rock and Lu-Hf in zircon)corroborate the restricted juvenile nature of the Mineiro Belt and confirm the genetic link between the Lagoa Dourada Suite,a rare ca. 2350 Ma high-Al tonalite-trondhjemite magmatic event, and the sanukitoid-type ca. 2130 Ma Alto Maranhao Suite. U-Pb dating of zircon and titanite constrain the crystallisation history of plutonic bodies; coupled with major and trace element analyses of the host rocks, they distinguish evolutionary trends in the Mineiro Belt. Several plutons in the region have ages close to 2130 Ma but are distinguished by the lower concentration of compatible elements in the juvenile high Ba-Sr suite. 相似文献
60.
Jurassic and Cretaceous (Yanshannian) tectonics,magmatism and metallogenesis in South China: preface
ABSTRACTSouth China is famous for its poly-metal deposits, with more than 50% of global W and Sb reserves, 20% of global Sn reserves, as well as abundant Cu-Mo-Pb-Zn-Au-Ag, Ta, Nb, REE and U deposits. This special issue consists of 21 papers, reporting recent progress on Yanshannian tectonic evolution, magmatism and ore deposits in South China, aiming at better understandings on the Mesozoic large-scale magmatism and mineralization events. 相似文献