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The dimension split element-free Galerkin method for three-dimensional potential problems 被引量:4
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作者 Z.J.Meng h.cheng +1 位作者 L.D.Ma Y.M.Cheng 《Acta Mechanica Sinica》 SCIE EI CAS CSCD 2018年第3期462-474,共13页
This paper presents the dimension split element-free Galerkin (DSEFG) method for three-dimensional potential problems, and the corresponding formulae are obtained. The main idea of the DSEFG method is that a three-d... This paper presents the dimension split element-free Galerkin (DSEFG) method for three-dimensional potential problems, and the corresponding formulae are obtained. The main idea of the DSEFG method is that a three-dimensional potential problem can be transformed into a series of two-dimensional problems. For these two-dimensional problems, the improved moving least-squares (IMLS) approximation is applied to construct the shape function, which uses an orthogonal function system with a weight function as the basis functions. The Galerkin weak form is applied to obtain a discretized system equation, and the penalty method is employed to impose the essential boundary condition. The finite difference method is selected in the splitting direction. For the purposes of demonstration, some selected numerical examples are solved using the DSEFG method. The convergence study and error analysis of the DSEFG method are presented. The numerical examples show that the DSEFG method has greater computational precision and computational efficiency than the IEFG method. 展开更多
关键词 Dimension split method Improved moving least-squares (IMLS) approximation Improved element-free Galerkin (IEFG) method Finite difference method (FDM) Dimension split element-free Galerkin (DSEFG) method Potential problem
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石笋记录的东亚季风气候H_1事件突变性特征 被引量:34
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作者 汪永进 刘殿兵 +4 位作者 吴金全 吴江滢 汪永进 蔡演军 h.cheng 《中国科学(D辑)》 CSCD 北大核心 2002年第3期227-233,共7页
据TIMS-U系测年和年纹层计数,建立了南京汤山葫芦洞一支石笋年际分辨率时间标尺(纹层计数年17451~14417aBP).石笋高分辨率氧同位素曲线揭示末次盛冰期东亚季风气候十年至百年尺度高频气温振荡特征,从中识别出响应于北大西洋最后一个H... 据TIMS-U系测年和年纹层计数,建立了南京汤山葫芦洞一支石笋年际分辨率时间标尺(纹层计数年17451~14417aBP).石笋高分辨率氧同位素曲线揭示末次盛冰期东亚季风气候十年至百年尺度高频气温振荡特征,从中识别出响应于北大西洋最后一个Heinrich(H1)事件的特强寒冷事件.该事件开始于16140±100aBP,并在此后36年内降温7~8℃.研究表明,事件所呈现的突发性降温形式以及跌宕式回暖过程(事件内部有10个冷暖旋回,并持续793a)主要受北半球中纬地区日辐照能背景、北大西洋冰漂碎屑带的扩张以及低纬太平洋海表温度变化诸因素的控制. 展开更多
关键词 石笋 东亚季风气候 H1事件 突变性
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