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41.
1991年江淮特大暴雨与东亚大气低频振荡   总被引:42,自引:3,他引:42  
陆尔  丁一汇 《气象学报》1996,54(6):730-736
本文分析了1991年江淮特大暴雨期间东亚大气低频振荡活动。从低频振荡特征看,江淮雨量和东亚风场中低频振荡现象是普遍存在的,风场的振荡周期具有显著的地域和频域分布特征。从低频波的传播看,这一梅雨过程的两个异常阶段(5月下半月和7月上半月),东亚风场低频波的水平传播方向发生了显著的变化。分析指出,低纬地区低频波虽有不同传播方向,但都将暖湿空气以低频形式输送到江淮以南,它与北侧的低频冷空气在江淮地区相互作用,从而导致该地区以低频形式出现的3场特大暴雨。  相似文献   
42.
对M700TY电台所用双极天线在发送语言和数据信号时,干扰周围仪器设备的原因进行了分析。针对电台干扰周围仪器设备的各种传播途径差异,采取抑制电台干扰,首先是抑制干扰源的方法,收到了比较明显的效果  相似文献   
43.
本文利用30~60天带通滤波资料, 考察了不同季节印度洋—西太平洋区域对流活动季节内尺度变率的主要模态, 发现在不同季节赤道东印度洋(5°S~10°N, 70°E~100°E)和西北太平洋(5°N~20°N, 110°E~160°E)对流活动均存在反相变化的关系, 将之称为季节内尺度的印度洋—西太平洋对流涛动(Indo-West Pacific Convection Oscillation), 简称IPCO。对IPCO两极子区域对流活动进行超前滞后相关分析, 发现IPCO事件形成—发展—消亡的生命周期是由对流活动季节内振荡及其传播造成的。对流扰动首先在赤道中西印度洋形成, 随后逐渐向东发展变强, 在其继续变强的过程中将分两支传播:一支由赤道印度洋向北传播, 至印度半岛南部后逐渐减弱消失;另一支沿赤道继续东传, 在海洋大陆受到抑制, 快速越过海洋大陆到达赤道西太平洋后又开始发展变强, 随后北传至西北太平洋区域逐渐减弱, 最终至我国长江流域中下游到日本区域消失。将这一过程划分为8个位相, 详细分析了不同位相对应的环流场和降水场特征, 最后给出了IPCO事件演化示意图。  相似文献   
44.
The Milky Way is a spiral galaxy with (or without) a bar-like central structure. There is evidence that the distribution of suspected cosmic ray sources, such as supernova remnants, are associated with the spiral arm structure of galaxies. It is yet not clearly understood what effect such a cosmic ray source distribution has on the particle transport in our Galaxy. We investigate and measure how the propagation of Galactic cosmic rays is affected by a cosmic ray source distribution associated with spiral arm structures.We use the PICARD code to perform high-resolution 3D simulations of electrons and protons in galactic propagation scenarios that include four-arm and two-arm logarithmic spiral cosmic ray source distributions with and without a central bar structure as well as the spiral arm configuration of the NE2001 model for the distribution of free electrons in the Milky Way. Results of these simulation are compared to an axisymmetric radial source distribution. Also, effects on the cosmic ray flux and spectra due to different positions of the Earth relative to the spiral structure are studied.We find that high energy electrons are strongly confined to their sources and the obtained spectra largely depend on the Earth’s position relative to the spiral arms. Similar finding have been obtained for low energy protons and electrons albeit at smaller magnitude. We find that even fractional contributions of a spiral arm component to the total cosmic ray source distribution influences the spectra on the Earth. This is apparent when compared to an axisymmetric radial source distribution as well as with respect to the Earth’s position relative to the spiral arm structure. We demonstrate that the presence of a Galactic bar manifests itself as an overall excess of low energy electrons at the Earth.Using a spiral arm geometry as a cosmic ray source distributions offers a genuine new quality of modeling and is used to explain features in cosmic ray spectra at the Earth that are else-wise attributed to other propagation effects. We show that realistic cosmic ray propagation scenarios have to acknowledge non-axisymmetric source distributions.  相似文献   
45.
大气Rossby波动力学的研究进展   总被引:5,自引:0,他引:5  
谭本馗 《气象学报》2008,66(6):870-879
Rossby波是旋转大气和海洋中的一类重要波动,在天气和气候演变中起有重要的作用。该文介绍了北半球中纬度地区的两类重要Rossby波——斜压不稳定波和准定常行星波,在最近20余年来取得的一些重要研究进展。文中涉及的主要研究领域有:斜压不稳定波包动力学、湿斜压过程对斜压不稳定波的作用、北半球风暴轴动力学、斜压波包与高影响天气的预报、准定常行星波的形成机理、准定常行星波的水平传播与能量频散、准定常行星波的垂直传播与能量频散、三维准定常行星波的传播与能量频散。  相似文献   
46.
列车引起场地振动的建模需要能够表达地层的动力格林函数.本文兼顾饱和土的流固两相耦合性、场地土的分层性和波动的三维传播性,构建了半解析的场地动力格林函数.首先,基于Biot方程,在傅里叶变换域求解固体骨架和流体的位移和应力.然后采用传递矩阵方法建立地表位移和应力间的关系,得到格林函数矩阵.进而讨论矩阵的一些固有特征,提出改善竖向位移计算效率的措施.最后利用推导的格林函数计算了几个典型算例.数值结果与文献中其他方法得到的结果十分接近,与场地振动的现场观测试验基本符合.软土场地振动的计算结果高于饱和砂土场地,高速列车场地振动强度高于低速列车.当车速接近场地瑞利波速,模拟结果中显示出马赫锥.数值结果还显示,即使车速略低于瑞利波速,马赫锥也可能出现.本文推导的格林函数将有助于深入理解列车等移动激励作用下层状饱和土场地的振动特征.  相似文献   
47.
An approach for simulating near-fault ground motion was presented by combining the finite fault model with a numerical algorithm, named investigated lump method presented in this paper for wave propagation. The investigated lumps are constructed from the auxiliary quadrilateral grids. The dynamic equilibrium equations of a typical investigated lump have been derived and obtained by integrating the stresses along the contour of the investigated lump. The stresses are calculated using the constitutive relations and the interpolation techniques. The investigated lump method is then implemented using the equilibrium equations of investigated lumps and the calculations of stresses alternately in time domain. The stability criterion of the algorithm has been given. Comparisons with the discrete wave-number method solutions for predicting the ground motions at the Pacoima Dam during the San Fernando earthquake show the validity of the method presented in this paper for simulating near-field ground motions. A finite fault source model has been implemented in the algorithm here. The source parameters given by Wald et al. (1996) [18] are applied to synthesize the ground motions at three stations during the 1994 Northridge earthquake. The simulating results qualitatively match to the corresponding ground motion records. The studies demonstrated that the approach presented in this paper is an effective tool for the numerical simulation of near-fault ground motion.  相似文献   
48.
Among the triggering factors of post-earthquake bedrock landslides,rainfall plays an important role.However,with slope variation,the mechanism of its effects on the failure of rock landslides is not clear.Here,from the viewpoint of fracture mechanics,and based on post-earthquake conditions,the mechanisms of crack propagation,water infiltration and development of the sliding surface were investigated.Then,according to the upper boundary theorem,the effects of water infiltrated into fractures on the stability of rock slopes were analyzed quantitatively.Finally,an example is presented to verify the theory.The results show that the propagation and coalescence of cracks and the lubrication of incipient sliding surfaces are the main causes of the failure of post-earthquake rock landslides in response to rainfall.  相似文献   
49.
This paper reviewed studies on remote sensing of water depth retrieval. Four water depth retrieval models (single-band, dou- ble-ratio-band, multi-band, and BP network models) were evaluated using TM image and water data from Bangong Co Lake, which is located in China's Tibet Autonomous Region and Indian Kashmir. Tested by independent data, comparison of these four models demonstrates that BP network model performed better than the multi-band model, with the single-band model performing the worst. To sum up, this study demonstrates that first, BP network model performed better than the traditional model; second, precise atmospheric correction and radiation study, affected by different water level sand sediment, could improve the precision of water depth retrieval.  相似文献   
50.
K-Ar和40Ar/39Ar定年数据质量评价与Q值提出   总被引:2,自引:2,他引:0  
K-Ar和K-Ar/39Ar的定年测试质量的评价是正确运用测试结果的前提.过去的研究,多通过仪器测试的偏差和误差传递来评价测试结果可靠性和精度.MSWD和Probability的提出,给出测试的内外误差概念,因考虑了仪器和样品二者的匹配性而得到广泛应用.这也说明,影响K-Ar和40Ar/39 Ar的定年测试结果的因素可以是来自仪器设备,也可以来自样品自身的特性.本文由K-Ar和40 Ar/39 Ar的定年技术的原理、流程为出发点,通过对各个测试项的误差传递和对结果精度影响的数学方法评估,提出了影响测试精度的Q1和Q2参数,分别代表与样品有关的属性.Q1是样品钾含量、囚禁36 Ar的含量、以及样品40Ar/36Ar的初始比值的综合参数,是决定仪器测试中误差传递系数大小的重要影响因子.Q2是样品钾含量、囚禁36 Ar的含量、以及样品40 Ar/36 Ar的初始比值误差的综合参数,用来评价样品等时线年龄精度.在地质意义上,Q2是评价样品是否满足“同源、同时、封闭”特性的重要量化指标.根据这两个参数,可以判别测试数据质量优劣是源于测试仪器,还是样品属性.由Q1和Q2的分析可知,任何一项K-Ar和40Ar/39 Ar的定年测试都应该充分考虑仪器性能和样品属性,设计合理的测试流程是K-Ar和40 Ar/39 Ar的定年获得较高质量数据的关键.  相似文献   
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