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Interactive multigraph visualization and exploration with a two-phase strategy 被引量:1
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作者 Huaquan Hu Lingda Wu +1 位作者 Chao Yang hanchen song 《Journal of Systems Engineering and Electronics》 SCIE EI CSCD 2014年第5期886-894,共9页
While it is very reasonable to use a multigraph consisting of multiple edges between vertices to represent various relationships, the multigraph has not drawn much attention in research. To visualize such a multigraph... While it is very reasonable to use a multigraph consisting of multiple edges between vertices to represent various relationships, the multigraph has not drawn much attention in research. To visualize such a multigraph, a clear layout representing a global structure is of great importance, and interactive visual analysis which allows the multiple edges to be adjusted in appropriate ways for detailed presentation is also essential. A novel interactive two-phase approach to visualizing and exploring multigraph is proposed. The approach consists of two phases: the first phase improves the previous popular works on force-directed methods to produce a brief drawing for the aggregation graph of the input multigraph, while the second phase proposes two interactive strategies, the magnifier model and the thematic-oriented subgraph model. The former highlights the internal details of an aggregation edge which is selected interactively by user, and draws the details in a magnifying view by cubic Bezier curves; the latter highlights only the thematic subgraph consisting of the selected multiple edges that the user concerns. The efficiency of the proposed approach is demonstrated with a real-world multigraph dataset and how it is used effectively is discussed for various potential applications. 展开更多
关键词 visual analytics information visualization multigraph visualization multiple edges aggregation graph magnifier model.
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古生代-中生代之交的水循环演变及驱动机制 被引量:3
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作者 宋汉宸 宋海军 +3 位作者 张仲石 吴玉样 楚道亮 舒文超 《科学通报》 EI CAS CSCD 北大核心 2023年第12期1501-1516,共16页
水循环是连接大气圈、水圈、岩石圈和生物圈的重要物质循环过程.本文根据地质记录和深时气候模拟等数据总结了古生代-中生代之交的水循环演变.结果表明,水循环在晚古生代、早中生代发生了重大变化:(1)地质记录恢复的气候带显示,当时全... 水循环是连接大气圈、水圈、岩石圈和生物圈的重要物质循环过程.本文根据地质记录和深时气候模拟等数据总结了古生代-中生代之交的水循环演变.结果表明,水循环在晚古生代、早中生代发生了重大变化:(1)地质记录恢复的气候带显示,当时全球的干旱带发生了明显扩张,蒸发岩面积从中-晚二叠世开始扩张,到早三叠世达到顶峰,中三叠世恢复至中-晚二叠世的水平,晚三叠-早侏罗世继续收缩;(2)全球年平均降水量在晚石炭、早侏罗世较高,中-晚二叠世和早三叠世较低,呈现为“V”字形变化,显示出一次重大的波动;(3)全球大陆的聚合可能导致泛大陆巨型陆面风和特提斯区域跨赤道风的形成,进而构成全球性的超级季风;(4)热带辐合带摆动的纬度位置在志留纪-石炭纪以及侏罗纪-现代较低,在二叠纪-三叠纪时期向高纬度大幅度漂移.根据事件发生的时间,这些水循环的重大变化与泛大陆的聚合、华力西造山、晚古生代冰期的结束以及大量碳释放和升温事件吻合,这些因素与当时的大气环流和水循环的变化存在密切联系:泛大陆的聚合改变了当时水储量的空间分布,同时改变了大气环流和“季风”,进而导致中-晚二叠世干旱带开始扩张,降水量减少;晚古生代末期华力西造山运动的减弱增强了热带辐合带的摆动,促进了超级季风的发展;碳释放驱动的升温事件改变了能量传输,影响了大气环流;同时植物面貌的转变影响了碳释放,进而影响水循环.由此可见,古生代-中生代之交水循环的强烈波动可能是该重大地质历史转折期岩石圈(地球深部过程)、大气圈(大气过程)、水圈(水循环)及生物圈(生命活动)相互作用的重要体现. 展开更多
关键词 热带辐合带 降水 超级季风 泛大陆聚合 干旱带扩张
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