北大西洋涛动指数的比较及其年代际变率

首先对各种北大西洋涛动（NAO）指数的定义进行了比较。发现冬季和夏季NAO的涛动中心有显著的差异,所以分别进行定义,定义时的中心由EOF分析及相关分析确定,新的定义能解释更多的海平面气压方差。在此基础上建立了1873年以来的冬、夏NAO指数序列。近百年来的NAO指数最突出的年代际变化是,夏季在1910～1920年期间的突变性质的增强,以及冬季近20多年来的持续加强。最后还对NAO年代际变化产生的可能原因进行了分析。     

秋季层状云中高值过冷水区的微物理特征

利用１１架次的机载“ＰＭＳ”资料,分析了山东秋季层状云中高值（大于０．１ｇ·ｍ~(－３)）过冷水区的微物理特征：最大过冷水含量为０．３６１ｇ·ｍ~(－３),８４．０％的过冷水含量在０．１～０．２ｇ·ｍ~(－３)间,过冷水连续出现的宽度８６．１％小于３．０ｋｍ。雪晶形状以霰粒和小雪粒为主。２阶(函数可以很好地拟合云滴尺度谱,质量谱适合用对数正态函数拟合。     

Spring Arctic Oscillation-East Asian summer monsoon connection through circulation changes over the western North Pacific

In the present study the links between spring Arctic Oscillation (AO) and East Asian summer monsoon (EASM) was investigated with focus on the importance of the North Pacific atmospheric circulation and sea surface temperature (SST). To reduce the statistical uncertainty, we analyzed high-pass filtered data with the inter-annual time scales, and excluded the El Ni?o/Southern Oscillation signals in the climate fields using a linear fitting method. The significant relationship between spring AO and EASM are supported by the changes of multi-monsoon components, including monsoon indices, precipitation, and three-dimensional atmospheric circulations. Following a stronger positive spring AO, an anomalous cyclonic circulation at 850?hPa appears in southeastern Asia and the western North Pacific in summer, with the easterly anomalies spanning from the Pacific to Asian continent along 25°N?C30°N and the westerly anomalies south of 15°N. At the same time, the summer western North Pacific subtropical high becomes weaker. Consistently, the positive precipitation anomalies are developed over a broad region south of 30°N stretching from southern China to the western Pacific and the negative precipitation anomalies appear in the lower valley of the Yangtze River and southern Japan. The anomalous cyclone in the western North Pacific persisting from spring to summer plays a key role in modulating EASM and monsoon precipitation by a positive air-sea feedback mechanism. During spring the AO-associated atmospheric circulation change produces warmer SSTs between 150°E?C180° near the equator. The anomalous sensible and latent heating, in turn, intensifies the cyclone through a Gill-type response of the atmosphere. Through this positive feedback, the tropical atmosphere and SST patterns sustain their strength from spring to summer, that consequently modifies the monsoon trough and the western North Pacific subtropical high and eventually the EASM precipitation. Moreover, the SST response to AO-circulation is supported by the numerical simulations of an ocean model, and the anomalous atmospheric circulation over the western North Pacific is also reproduced by the dedicated numerical simulations using the coupled atmosphere?Cocean model. The observation evidence and numerical simulations suggest the spring AO can impact the EASM via triggering tropical air-sea feedback over the western North Pacific.     

水汽瞬态相变的激波管实验研究进展

从激波管内水汽瞬态相变实验研究的角度出发，探讨利用激波管理论及实验技术应用于人工影响降雨、消雹所涉及的云雾瞬态相变问题。首先介绍利用激波管研究水汽瞬态相变的概况，并介绍一些特殊激波管及实验状态的控制。然后介绍激波管内水汽相变过程研究的测试原理及方法。最后讨论在研究爆炸方法进行人工降雨、消雹和自然闪电、雷击等问题时，应用激波管理论及实验技术进行实验研究爆炸作用于云雾等微物理过程的方法和内容     

Research on the security of national geospatial data clearinghouse based on ASP

1　ＩｎｔｒｏｄｕｃｔｉｏｎＮｅｅｄｌｅｓｓｔｏｓａｙ ,ｉｔｉｓｖｅｒｙｉｍｐｏｒｔａｎｔｆｏｒｍｏｓｔＧＩＳｕｓｅｒｓｔｏａｃｑｕｉｒｅａｎｄｉｎｔｅｇｒａｔｅｔｈｅｇｅｏｓｐａｔｉａｌｉｎｆｏｒ ｍａｔｉｏｎｆｒｏｍｖａｒｉｏｕｓｄｉｓｔｒｉｃｔｓ.Ｈｏｗｅｖｅｒ ,ｔｈｅｃｕｒｒｅｎｔｓｉｔｕａｔｉｏｎｏｆｇｅｏｓｐａｔｉａｌｉｎｆｏｒｍａｔｉｏｎｐｒｏｄｕｃｔｉｏｎａｎｄｄｉｓｓｅｍｉｎａｔｉｏｎｉｎｔｈｅｗｏｒｌｄｉｓｓｔｉｌｌｕｎｓａｔｉｓｆａｃｔｏｒｙ .Ｏｎｏｎｅｈａｎｄ ,ｕｓｅｒｓｄ…     

三类降水云雨滴谱分布模式

利用沈阳１９９４年７～８月雨滴谱观测资料,进行积雨云、层状云和积层混合云Ｍ－Ｐ分布和Γ分布拟合分析,讨论了两种分布适用范围,给出了分布参数随雨强变化关系。     

关于发展我国地下流体前兆流动观测问题的建议

从主机故障、传感器故障、避雷系统故障、供电系统故障4个方面,对天津流体台网水温观测系统故障事件及其跟踪分析进行讨论,提出规范化的排查思路及记录处理方法,可供兄弟台站作为同类数据跟踪分析工作的参考。     

Validating the ability of the discontinuous deformation analysis method to model normal P‐wave propagation across rock fractures

The effects of fractures on wave propagation problems are increasingly abstracting the attention of scholars and engineers in rock engineering field. This study aims to fully validate the ability of discontinuous deformation analysis (DDA) to model normal P‐wave propagation across rock fractures. The effects of a single fracture and multiple parallel fractures are all tested. The results indicate that DDA can accurately reflect the fracture effects, including the fractures stiffness, the fracture spacing and the fracture number, and the effects of incident wave frequency on one‐dimensional P‐wave propagation problems. Thus, DDA is able to deal well with normal incident P‐wave propagation problems. Copyright © 2017 John Wiley & Sons, Ltd.