Possible Impacts of the Arctic Oscillation on the Interdecadal Variation of Summer Monsoon Rainfall in East Asia

The influences of the wintertime AO (Arctic Oscillation) on the interdecadal variation of summer monsoon rainfall in East Asia were examined. An interdecadal abrupt change was found by the end of the 1970s in the variation of the AO index and the leading principal component time series of the summer rainfall in East Asia, The rainfall anomaly changed from below normal to above normal in central China, the southern part of northeastern China and the Korean peninsula around 1978. However,the opposite interdecadal variation was found in the rainfall anomaly in North China and South China.The interdecadal variation of summer rainfall is associated with the weakening of the East Asia summer monsoon circulation. It is indicated that the interdecadal variation of the AO exerts an influence on the weakening of the monsoon circulation. The recent trend in the AO toward its high-index polarity during the past two decades plays important roles in the land-sea contrast anomalies and wintertime precipitation anomaly. The mid- and high-latitude regions of the Asian continent are warming, while the low-latitude regions are cooling in winter and spring along with the AO entering its high-index polarity after the late 1970s. In the meantime, the precipitation over the Tibetan Plateau and South China is excessive, implying an increase of soil moisture. The cooling tendency of the land in the southern part of Asia will persist until summer because of the memory of soil moisture. So the warming of the Asian continent is relatively slow in summer. Moreover, the Indian Ocean and Pacific Ocean which are located southward and eastward of the Asian land, are warming from winter to summer. This suggests that the contrast between the land and sea is decreased in summer. The interdecadal decrease of the land-sea heat contrast finally leads to the weakening of the East Asia summer monsoon circulation.     

HCl Quasi-Biennial Oscillation in the Stratosphere and a Comparison with Ozone QBO

1. Introduction The quasi-biennial oscillation (QBO) of the mean zonal wind in the equatorial stratosphere was discov- ered by Reed et al. (1961) and Veryard and Ebdon (1961). Later, Funk and Garnham (1962) and Ra- manathan (1963) were the first to descri…     

电磁式可控震源-大地耦合过程中的非线性特征分析

基于液压式可控震源的线性模型在电磁式可控震源的应用上已不再适合, 故电磁式可控震源-大地耦合模型研究对实现有限激励能量向大地的最佳传输至关重要. 由于可控震源基板中含有大量高频谐波, 在耦合模型中引入非线性恢复力, 并通过用多尺度法对系统进行了非线性振动分析. 对振动过程中的超谐共振现象为能量传输过程中谐波的产生给出了合理的解释, 并为可控震源地震勘探中互相关参考信号的选取提出了改进方案, 通过野外实验, 取得了良好的应用效果.     

《地震工程与工程振动》、《自然灾害学报》荣获首届黑龙江省出版精品工程奖提名奖

由黑龙江省省委宣传部、省新闻出版局共同组织的首届黑龙江省出版精品工程奖评选工作日前结束。共有三大门类（图书、社科期刊、科技期刊）93种出版物分获精品工程特别奖、精品工程奖和精品工程提名奖。由中国地震局工程力学研究所主办的《地震工程与工程振动》和《自然灾害学报》荣获首届黑龙江省出版精品工程奖提名奖。     

北京地铁光华路站风道暗挖工程监控量测技术

结合北京地铁光华路站西北风道工程施工中应用的监控量测系统技术，介绍城市地铁工程施工中如何通过监测地表沉降、拱顶沉降等来控制和指导施工。     

秩亏自由网平差在地铁隧道保护区中的应用

地铁隧道保护区沉降监测网中包含多个基准点,依据不同基准点平差所得结果也不相同。本文引入秩亏自由网平差方法,将所有基准点视为待定参数进行平差,并通过工程实例,验证此方法在地铁隧道保护区沉降观测中有一定的适用性。     

地铁车站群洞效应下变形监测研究

结合重庆地铁6号线金山寺车站群洞开挖施工背景,对车站结构、地质条件和施工方法等工况分析后,提出了该工况下变形监测基本思想。确定了监测项目、监测点位布设方案、监测方法及监测数据分析方法,初步制定了监测信息反馈流程。依此思想进行变形监测并及时、有效地反馈监测信息,可保证群洞开挖安全、顺利进行。     

基于灰色支持向量机的地铁沉降滚动预测

为了确保地铁隧道主体结构和周边环境安全,必须对地铁隧道结构进行沉降监测,对监测数据进行及时分析与反馈,并对以后的沉降情况作出预测,对防止事故发生有着重要的现实意义。本文结合灰色系统理论和支持向量机(SVM)的基本原理,采用滚动预测的方式建立灰色支持向量机沉降预测模型,以提高沉降预测精度。通过工程实例的预测结果对比表明,组合模型与灰色和SVM两个单独预测模型相比能够更准确的反映实际的沉降过程,具有很大的应用价值。     

航空重力仪减振系统振动研究

航空重力减振系统是有效减弱机载环境下高频振动的主要途径,从而提高航空重力的测量精度。因此,设计减振系统的首要问题是设定其合理的刚度、阻尼和质量等重要的特性参数。笔者通过建立航空重力仪两种减振系统类型运动微分方程,经过理论和实例探讨了减振系统模型,旨在深入了解航空重力减振系统的减振规律,为其特性参数设计提供理论依据。     

横向振动格栅紊流紊动特性试验

建立了一套大尺度格栅紊流试验系统,格栅进行有别于传统垂向模式的横向振动,采用粒子图像测速技术(Particle Image Velocimetry,PIV)测量流速。对瞬时流速的检验表明,该系统产生的紊流场具有较强的随机性和统计规律性。均方根流速在格栅片附近变化较大,在两片格栅中间处趋于稳定,纵向均方根流速明显大于垂向均方根流速,二者比值在1.5~2.0之间,接近天然明渠紊流。雷诺应力在距格栅越近处波动越大,随着距格栅距离的增加而减小,至两片格栅中间处雷诺应力基本为0。时间和长度积分尺度在格栅片处最小,随着距格栅距离的增加而线性增加,至两片格栅中间处达到最大值。流速能谱呈现Kolmogorov理论的-5/3次方规律。本系统生成的紊流场的统计规律与传统的垂向振动格栅紊流较为一致,但纵向和垂向的紊动强度更接近实际,为后续紊流中泥沙和污染物等运动机理的研究奠定了基础。