Visualization in the Earth Sciences: A Discussion on Various Visualization Methods using amira

S. Wang, M. Damon, D. Yuen
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引用次数: 3

Abstract

It is widely acknowledged that an important aspect in Earth Science research is the ability to visualize huge amounts of data resulting from numerical simulations or data acquisition. Whether the data is a simple two-dimensional plot or a three-dimensional multivariate grid, the ability to visualize the data is imperative for researchers to properly demonstrate results. This poster will examine various visualization techniques of the software package, amira® (www.amiravis.com) with respect to three research projects. These projects are: a mantle convection simulation run on the Earth Simulator; a spherical harmonic model computed at the University of Minnesota's Supercomputing Institute; an upper mantle study of earthquake-generated shear waves down to 660 km obtained through computed tomography using seismogram data from the Incorporated Research Institutions for Seismology (IRIS). The data resulting from the mantle convection study is in the form of a regular cartesian grid consisting of various field parameters such as temperature, velocity and viscosity. Techniques employed to view these fields include but are not limited to volume rendering, illuminated streamlines and oblique slices. The spherical harmonics model is rendered as a volume and is also explored using an isosurface module. The upper mantle study is visualized using an oblique slice technique and also isosurfaces. An analysis of the benefits and drawbacks of various amira® modules in regard to the above projects will not only result in a better understanding of the data, but will also demonstrate the unique capabilities of the different techniques and how they can be best applied to specific problems in the Earth Sciences.
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地球科学中的可视化:利用amira的各种可视化方法的讨论
人们普遍认为,地球科学研究的一个重要方面是能够将由数值模拟或数据采集产生的大量数据可视化。无论数据是简单的二维图还是三维多元网格,可视化数据的能力对于研究人员正确展示结果是必不可少的。这张海报将检查软件包的各种可视化技术,amira®(www.amiravis.com)与三个研究项目有关。这些项目是:在地球模拟器上运行的地幔对流模拟;明尼苏达大学超级计算研究所计算的球谐模型;利用地震学联合研究机构(IRIS)的地震记录数据,通过计算机断层扫描,对660公里以下地震产生的横波进行了上地幔研究。地幔对流研究得到的数据是由温度、速度和粘度等各种场参数组成的规则笛卡尔网格。用于查看这些领域的技术包括但不限于体积渲染、照明流线和斜切片。球面谐波模型被渲染为一个体,并且还使用一个等面模块进行了探索。上地幔研究使用斜切片技术和等值面进行可视化。对上述项目中各种amira®模块的优缺点进行分析,不仅可以更好地理解数据,还可以展示不同技术的独特功能,以及如何将它们最好地应用于地球科学中的具体问题。
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