乌鲁木齐市PM10,PM2.5和PM1.0浓度及分布变化特征研究     

韩茜  魏文寿  刘新春  钟玉婷 《沙漠与绿洲气象(新疆气象)》2015,9(1):32-38

利用GRIMM180气溶胶粒谱分析仪采集乌鲁木齐市PM10、PM2.5和PM1.0数据,研究表明:乌鲁木齐市气溶胶颗粒物质量浓度在进入采暖季后急剧增加,冬季颗粒物中细粒子含量最高,PM2.5/PM10可达77.6%,PM2.5/PM10,PM1.0/PM10,PM1.0/PM2.5三比值体现了颗粒物的分布特征,四季污染程度越高,细粒子含量越高。四季无降水日PM10、PM2.5、PM1.0的质量浓度和分布的日变化基本呈三峰三谷型,出现早—午—晚峰值,上午—下午—午夜后谷值,各季节峰谷值具体出现时间略有差别,由于冬季逆温层顶盖等因素的影响,冬季质量浓度和分布的日变化在此基础上多了两次波动。降水的发生对冬、春季质量浓度的影响大于夏、秋季,对不同粒径段粒子的分布影响有一定差别。  相似文献   

海温异常对东亚夏季风强度先兆信号的影响   总被引：1，自引：1，他引：0       下载免费PDF全文

柯宗建  华丽娟  钟霖浩  杜良敏 《应用气象学报》2015,26(5):536-544

利用ERA-Interim再分析资料、NOAA海温资料、CMAP格点降水资料和中国气象站降水资料,通过合成、相关和回归分析等方法研究了1979—2012年东亚夏季风强度与其先兆信号的关系,并分析了热带海温异常的可能影响。研究表明:东亚夏季风先兆指数反映了2月200 hPa纬向风距平的主要模态特征 (EOF1),前冬热带中东太平洋海温偏低 (高),2月亚洲地区西风急流位置偏北 (偏南),东亚夏季风先兆指数偏强 (弱)。前期热带海温异常对东亚夏季风强度有明显影响,前冬热带中东太平洋海温偏低 (高) 有利于东亚夏季风偏强 (弱)。2月亚洲中纬度地区纬向风异常特征在春季不能持续,先兆信号与东亚夏季风强度的联系主要源自热带海洋。  相似文献   

基于GIS的广西电网流域面雨量计算方法与监测预警     

钟利华  钟仕全  曾鹏  袁丽军  李勇 《气象研究与应用》2015,36(1)

以广西电网直调水电厂所处的西江流域为研究对象,基于GIS技术,在对西江流域面雨量监测区域基础信息处理基础上,采用比较分析方法,开展分流域面雨量计算方法研究,结果表明:(1)以1:5万数字高程模型为数据基础,针对西江流域河网、自动气象站、水电站等分布特点,结合水系、等高线特征,沿水系分水岭对西江流域干流进行精细化分区,为分流域面雨量计算提供基础参数;(2)对分流域面雨量采用算术平均法与泰森多边形法计算,结果为两种方法计算结果偏差较小,取算术平均法为流域分区面雨量计算方法;(3)逐小时处理、计算面雨量实时数据,实现西江流域面雨量的实时监测与预警服务。  相似文献   

一致性哈希算法在数据库集群上的拓展应用     

赵飞  苏忠 《成都信息工程学院学报》2015,30(2)

在数据库集群的研究中,可扩展性是一个重要的性能指标.为实现在数据高速增长或部分集群服务器故障情况下,数据依然能够快速、可靠、安全的分布到新的集群服务器节点上的目的,就必须合理设置数据划分的策略.将Key-Value存储技术中使用的一致性哈希算法思想借鉴运用到并行分析型数据库集群中,提出针对大规模结构化类特殊数据的一致性哈希划分方法,并在MapReduce框架下设计具体的数据划分方案.最后,以TPC-DS作为测试基准,与同类系统进行性能对比测试,实验结果表明方案不仅有良好的划分性能,且扩展性也较好.  相似文献   

一致性哈希算法在数据库集群上的拓展应用   总被引：2，自引：0，他引：2  

赵飞  苏忠 《成都信息工程学院学报》2015,30(1):52-58

在数据库集群的研究中,可扩展性是一个重要的性能指标。为实现在数据高速增长或部分集群服务器故障情况下,数据依然能够快速、可靠、安全的分布到新的集群服务器节点上的目的,就必须合理设置数据划分的策略。将Key-Value存储技术中使用的一致性哈希算法思想借鉴运用到并行分析型数据库集群中,提出针对大规模结构化类特殊数据的一致性哈希划分方法,并在MapReduce框架下设计具体的数据划分方案。最后,以TPC-DS作为测试基准,与同类系统进行性能对比测试,实验结果表明方案不仅有良好的划分性能,且扩展性也较好。  相似文献   

Application of Spatial Database in Quantitative Analysis of Litho-Paleogeography—A Case Study of a Middle Ordovician Sequence Interval in the Ordos Basin     

Bin Li  Feiyan Liao  Hao Meng  Yanchun Zhong 《地球空间信息科学学报》2011,14(1):27-38

In the study of sequence stratigraphy and litho-paleogeography,quantitative analysis,precise calculation and detailed comparison of tremendous geological data,such as field profiles,logging records and seismic curves from different areas,are the basic requirements.In order to obtain a more reliable and precise result,this paper presents a novel method that combines spatial database analysis with the single-factor mapping technology to establish sequence stratigraphical succession and to map the Ordo-vician litho-paleogeography of the Ordos Basin,one of the largest oil-gas bearing basins in North China Platform.By using this method,all of the related basic geological data can be quantitatively analyzed and effectively managed.Various attributes of the ba-sic stratigraphic units and their characters,such as sequence thickness,penecontemporaneous dolostone content,shallow water parget content,and terrigenous material content,can be fully utilized statistically in facies analysis and in mapping.Based on this analysis,this paper has be exerted single-factor isopachous mapping quantitatively for each of the Ordovician sequences in the ba-sin,and finally synthesized multiple factors to reconstruct the litho-paleogeography for each of the sequence intervals.The study shows that the proposed method is quite effective and has a much higher resolution in recognizing litho-paleogeographic subunits compared with traditional ways.For example,in one of the Middle Ordovician sequence intervals(SQ19 in the Lower Majiagou Formation) of the Ordos Basin,the authors have successfully developed a mathematical formula to divide the distribution of various facies units substantially,such as old lands,submarine uplifts,supratidal zones,intertidal zones and subtidal zones.  相似文献   

空中三角测量中WuCAPS的应用     

魏忠  周军元  陈春华 《地理空间信息》2011,9(3):15-16

通过WuCAPSGPS加密方案与传统方案的比较,阐明了WuCAPSGPS加密方案在减少野外工作量,缩短成图周期方面的重要意义.  相似文献   

HBCORS省内区域分中心建设研究   总被引：1，自引：1，他引：0  

魏忠  高长元  李剑 《地理空间信息》2011,(5):18-19,22

加快区域分中心的建设,是确保湖北省连续运行卫星定位服务系统（简称HBCORS）稳定高效运行的重要因素。从湖北省实际情况出发,客观分析了湖北省现有参考站实际情况及面临的困难后,制定了一系列的区域分中心建设原则,并在此原则上,对省内区域分中心进行了有序布设,对各区域分中心在系统维护方面的主要职责进行了详细划分。  相似文献   

Centennial-scale climate change from decadally-paced explosive volcanism: a coupled sea ice-ocean mechanism   总被引：1，自引：1，他引：0  

Y. Zhong  G. H. Miller  B. L. Otto-Bliesner  M. M. Holland  D. A. Bailey  D. P. Schneider  A. Geirsdottir 《Climate Dynamics》2011,37(11-12):2373-2387

Northern Hemisphere summer cooling through the Holocene is largely driven by the steady decrease in summer insolation tied to the precession of the equinoxes. However, centennial-scale climate departures, such as the Little Ice Age, must be caused by other forcings, most likely explosive volcanism and changes in solar irradiance. Stratospheric volcanic aerosols have the stronger forcing, but their short residence time likely precludes a lasting climate impact from a single eruption. Decadally paced explosive volcanism may produce a greater climate impact because the long response time of ocean surface waters allows for a cumulative decrease in sea-surface temperatures that exceeds that of any single eruption. Here we use a global climate model to evaluate the potential long-term climate impacts from four decadally paced large tropical eruptions. Direct forcing results in a rapid expansion of Arctic Ocean sea ice that persists throughout the eruption period. The expanded sea ice increases the flux of sea ice exported to the northern North Atlantic long enough that it reduces the convective warming of surface waters in the subpolar North Atlantic. In two of our four simulations the cooler surface waters being advected into the Arctic Ocean reduced the rate of basal sea-ice melt in the Atlantic sector of the Arctic Ocean, allowing sea ice to remain in an expanded state for?>?100 model years after volcanic aerosols were removed from the stratosphere. In these simulations the coupled sea ice-ocean mechanism maintains the strong positive feedbacks of an expanded Arctic Ocean sea ice cover, allowing the initial cooling related to the direct effect of volcanic aerosols to be perpetuated, potentially resulting in a centennial-scale or longer change of state in Arctic climate. The fact that the sea ice-ocean mechanism was not established in two of our four simulations suggests that a long-term sea ice response to volcanic forcing is sensitive to the stability of the seawater column, wind, and ocean currents in the North Atlantic during the eruptions.  相似文献   

Diagnostic Analysis of the Quasi-Balanced Flow of a Mesoscale Vortex During the 12 June 2008 Guangxi Rainstorm          下载免费PDF全文

GE Jingjing  ZHONG Wei  LU Hancheng 《Acta Meteorologica Sinica》2011,25(2):188-202

By using the high-resolution observation data and MM5 model simulation data, the analysis on the 12 June 2008 Guangxi flash-flood rainstorm shows that the associated major mesoscale weather system of this event is a quasi-stationary mesoscale vortex, which resulted from the interaction between the midlatitude synoptic-scale waves in the westerly belt and the low-latitude warm-moist flow under the terrain effect. The genesis, development, and movement of the mesoscale vortex have significant impacts on the intensity and persistence of the severe precipitation from the Guangxi flash-flood rainstorm. This vortex is characterized by the coexistence of strong vorticity and divergence with the same order of magnitude. Well organized, deep, and moist convection was observed for a long period of time, and was produced by the interaction between the mesoscale vortex and the gravity waves. The latter was generated by the terrain effect and the ageostrophic effect of high winds in the low-level jet. According to the quasi-balanced dynamical theory, quasi-balanced flow must have existed in the mesoscale motions with both divergent and rotational winds. Thus, based on the diagnosis of the quasi-balanced flow, the PV-ωinversion method is employed to analyze the organized moist convection. The results show that 50%-70% of the vertical circulation in the rainstorm areas was quasi-balanced, so the quasi-balanced flow could well reflect features of the strong vertical motions associated with the coexistence of vorticity and divergence during this event.  相似文献