在拖拽系统水动力理论研究的基础上,根据集中质量法建立曳纲的三维动力学数学模型,将曳纲在空间上离散为一系列节点,同时忽略曳纲的扭转、抖动等,计入张力、重力、浮力和流体阻力的作用,建立曳纲的动态运动数学模型,并通过四阶龙格库塔...在拖拽系统水动力理论研究的基础上,根据集中质量法建立曳纲的三维动力学数学模型,将曳纲在空间上离散为一系列节点,同时忽略曳纲的扭转、抖动等,计入张力、重力、浮力和流体阻力的作用,建立曳纲的动态运动数学模型,并通过四阶龙格库塔方法积分求解,得到曳纲的位置和速度信息,最后利用三维图形引擎OSG(Open Scene Graph)实现拖曳系统的三维可视化。数值计算结果与相关试验数据比较表明,曳纲模型的求解方法是可靠的,同时又保证了仿真的实时性。展开更多
Based on the pentad mean ridgeline index of the western Pacific subtropical high (WPSH), the authors identified the two northward jumps of the WPSH from 1979 to 2008 and revealed their associations with the tropical S...Based on the pentad mean ridgeline index of the western Pacific subtropical high (WPSH), the authors identified the two northward jumps of the WPSH from 1979 to 2008 and revealed their associations with the tropical SST anomalies. The authors show that the northward jumps, especially the second jump, exhibited remarkable interannual variability. In addition, the authors find that the two northward jumps were mutually independent and were influenced by the SST anomalies in the different regions of the tropical Pacific. The first jump was positively correlated with the SST anomalies in the tropical central Pacific from the preceding winter to June. In contrast, the second jump was positively related to ENSO in the preceding winter, but this correlation tended to weaken with the decay of ENSO and disappeared in July. Instead, a positive correlation was found in the Indian Ocean. We therefore suggest that ENSO plays an indirect role in the second jump through the capacitor effect of the Indian Ocean.展开更多
文摘在拖拽系统水动力理论研究的基础上,根据集中质量法建立曳纲的三维动力学数学模型,将曳纲在空间上离散为一系列节点,同时忽略曳纲的扭转、抖动等,计入张力、重力、浮力和流体阻力的作用,建立曳纲的动态运动数学模型,并通过四阶龙格库塔方法积分求解,得到曳纲的位置和速度信息,最后利用三维图形引擎OSG(Open Scene Graph)实现拖曳系统的三维可视化。数值计算结果与相关试验数据比较表明,曳纲模型的求解方法是可靠的,同时又保证了仿真的实时性。
基金supported by the National Basic Research Program of China(Grant No.2010CB951901)the National Natural Science Foundation of China(Grant No.40821092)
文摘Based on the pentad mean ridgeline index of the western Pacific subtropical high (WPSH), the authors identified the two northward jumps of the WPSH from 1979 to 2008 and revealed their associations with the tropical SST anomalies. The authors show that the northward jumps, especially the second jump, exhibited remarkable interannual variability. In addition, the authors find that the two northward jumps were mutually independent and were influenced by the SST anomalies in the different regions of the tropical Pacific. The first jump was positively correlated with the SST anomalies in the tropical central Pacific from the preceding winter to June. In contrast, the second jump was positively related to ENSO in the preceding winter, but this correlation tended to weaken with the decay of ENSO and disappeared in July. Instead, a positive correlation was found in the Indian Ocean. We therefore suggest that ENSO plays an indirect role in the second jump through the capacitor effect of the Indian Ocean.
