数字化建设用地动态监管系统的开发

数字化建设用地动态监管系统是一个基于网络的实时在线监管平台。本文系统的介绍了数字化建设用地动态监管系统的系统技术架构、系统功能设计、关键技术等,为数字化建设用地动态监管技术研究及应用提供借鉴。     

Antarctica Sea-ice Oscillation and Its Possible Impact on Monsoon of South Sea

Antarctic sea-ice oscillation index with a seesaw pattern is defined using NCEP/NCAR reanalysis girds data of monthly Antarctica sea-ice concentration from 1979 to 2002. The relationships between the index of winter and the summer precipitations in China as well as the onset date of the summer East Asia monsoon are presented. The study result shows that the grids of correlation coefficients passed 5% confidence level between Antarctic sea-ice oscillation index and Antarctic sea-ice concentration are more than 1/3 of all grids of Antarctica sea-ice, that means the index can represent 1/3 sea-ice area. The winter index has a significant correlation with abnormal summer (June-August) precipitation in China. The area of positive correlation lies in the Yangtze River basin and its south, and that of negative correlation lies mainly in the north of Yangtze River basin. While the winter index is positive (negative), the onset date of South China Sea monsoon is earlier (later), with a probability of 79% (80%). Consequently, a conceptual model is given in term of discussing the possible process between the winter Antarctic sea ice and the monsoon precipitation in China.     

Structure of summer atmospheric boundary layer in the center of Arctic Ocean and its relation with sea ice extent change

The atmospheric vertical structure and changed characteristics of boundary layer parameters, as well as their relations with sea ice and temperature changes in the center of Arctic Ocean(80°–88°N) are presented by adopting GPS sounding data obtained by the 4th–6th Arctic expeditions of China and NCEP(National Centre for Environmental Prediction) reanalysis data. Obvious differences are observed regarding the tropopause, boundary layer height, temperature inversion, and vertical structure of wind speed and direction in the center Arctic Ocean in the summer of 2012, 2010, and 2014. These differences can be explained by the relations between temperature and changes in sea ice extent in September from 1979 to 2014. In September 2012, the Arctic sea ice extent decreased by 44% an with obvious warming process. In September 2010 and 2014, it decreased by 22.6% and 17% with an obvious cooling process, respectively. A comparison of the two processes shows that sea ice change has a significant influence on the structure of the atmospheric boundary layer. In the recent 30 years, the temperature changes of 1000 and 850 h Pa in the center of the Arctic Ocean have displayed an obvious warming trend and negative correlation with sea ice extent. These changes indicate that the continuous reduction of Arctic sea ice will continue the warming of the troposphere middle layer.     

天津市地震局地震事件共享系统的设计与实现

分析了天津市测震台网历史数据的使用现状,并利用PHP语言和百度地图API程序的二次开发,建立了天津市地震局地震事件共享系统。利用该系统实现了天津市地震局历史地震事件的共享,用户可通过共享系统查询地震目录和下载地震事件,通过My Sql数据库语言设计系统各功能模块相关数据库表单,保存地震目录信息、用户反馈信息相关图片。该系统通过SESSION变量实现用户权限管理,避免了事件文件误传的可能性。通过该系统平台的投入使用,提升了系统原有地震事件保存方式,方便了用户查询使用事件文件的效率,使数据共享工作在天津市地震局得到了提升。     

分段压水试验在东平大牛矿区水文地质勘查中的应用

压水试验方法同样适用于矿区水文地质勘查的各阶段,特别是针对透水性不是很大的矿区,选择单管栓塞压水试验方法,有使用方便、操作简单、灵活易行、不受孔径限制等独具的特点。在同一钻孔中进行分段压水试验,计算各段的透水率、渗透系数,根据各段渗透性对矿区含水层、段进行划分,为矿区水文地质条件划分提供依据。     

Validation of global land surface satellite (GLASS) downward shortwave radiation product in the rugged surface

The downward shortwave radiation(DSR) is an essential parameter of land surface radiation budget and many land surface models that characterize hydrological,ecological and biogeochemical processes.The new Global LAnd Surface Satellite(GLASS) DSR datasets have been generated recently using multiple satellite data in China.This study investigates the performances of direct comparison approach,which is mostly used for validation of surface insolation retrieved from satellite data over the plain area,and indirect comparison approach,which needs a fine resolution map of DSR as reference,for validation of GLASS DSR product in time-steps of 1 and 3 hours over three Chinese Ecosystem Research Network sites located in the rugged surface.Results suggest that it probably has a large uncertainty to assess GLASS DSR product using the direct comparison method between GLASS surface insolation and field measurements over complex terrain,especially at Mt.Gongga 3,000 m station with root mean square error of 279.04 and 229.06 W/m2in time-steps of 1 and 3 hours,respectively.Further improvement for validation of GLASS DSR product in the rugged surface is suggested by generation of a fine resolution map of surface insolation and comparison of the aggregated fine resolution map with GLASS product in the rugged surface.The validation experience demonstrates that the GLASS DSR algorithm is satisfactory with determination coefficient of 0.83 and root mean square error of 81.91W/m2over three Chinese Ecosystem Research Network sites,although GLASS product overestimates DSR compared to the aggregated fine resolution map of surface insolation.     

EMC存储系统在天津测震台网JOPENS数据库服务中的应用

主要阐述EMC存储系统在天津测震台网的JOPENS数据库服务中的应用情况,对采用本地存储、EMC SATA硬盘和EMC光纤硬盘存储进行了分析对比,为现存的基于本地存储模式的测震台网JOPENS数据库服务器扩展到统一数据存储模式做示范;为省级区域中心进行统一的数据存储应用环境提供参考.     

全球冰冻圈变化预测研究现状

冰冻圈是气候系统重要的圈层,对气候系统有强烈的反馈作用,在全球变暖的背景下,冰冻圈的变化和预测研究愈来愈受到科学界的重视。近年来,冰冻圈的预测研究已经取得重要进展,主要表现在:海冰、积雪冻土等子系统模式发展迅速,开展了不少模式比较计划,这些模式能重现大尺度的季节变化和年际变化特征,模拟能力较以前有了大幅度提高。但模式模拟的不确定性仍普遍存在,主要表现在:冰盖等子系统的模式对于其内部的热力过程、其底部与海洋的相互作用过程缺乏有效的观测手段,认识不够清楚,湖冰河冰模式主要还依赖统计相关模型。随着遥感技术以及资料同化技术的不断应用,各个子系统物理过程认识的不断深入,冰冻圈模式预测将日趋完善,逐渐缩小不确定性。     

积雪对南极冰盖自动气象站气温观测影响的研究

随着冰盖表面雪的累积或消融,自动气象站(AWS)传感器相对地表的高度随之发生变化,故所记录的观测资料不能直接反映相对地表固定高度上的气象参数。为了使南极冰盖上AWS所获取的气象资料具有可靠性,在积累率对AWS观测气温影响的基础上,将东南极冰盖上中山站至DomeA断面3个AWS的连续观测气温修正到相对于雪表面的某一真实高度上。结果表明:(1)DomeA,Eagle和LGB69年平均1m气温分别为-53.19℃,-41.33℃和-26.29℃,年平均积累率分别为0.11m、0.30m和0.49m,对应的1m气温年平均修正量分别为0.34℃、0.29℃和0.35℃,2m和4m气温的年平均修正量均小于0.1℃;(2)积累率变化对离地表最近层次上的气温影响最大,越往上层影响越小;(3)气温的修正量大小与积累率并非成简单的正比关系,它与气温本身的季节变化特征以及局地近地表逆温强度有很大的关系。气温的平均修正量冬季为正,夏季修正量的正负由局地是否存在逆温决定,修正量值的大小主要由逆温强度和积累率决定。     

Radio Luminosity, Black Hole Mass and Eddington Ratio for Quasars from the Sloan Digital Sky Survey

We investigate the MBH-O'.relation for radio-loud quasars with redshift z＜0.83 in Data Release 3 of the Sloan Digital Sky Survey (SDSS).The sample consists of 3772 quasars with better models of the H/~ and [O III] lines and available radio luminosity,including 306 radio-loud quasars,3466 radio-quiet quasars with measured radio luminosity or upper-limit of radio luminosity (181 radio-quiet quasars with measured radio luminosity).The virial supermassive black hole mass (MBH) is calculated from the broad H/line,and the host stellar velocity dispersion (σ*) is traced by the core [O III] gaseous velocity dispersion.The radio luminosity and radio loudness are derived from the FIRST catalog.Our results are as follows:(1) For radio-quiet quasars,we confirm that there is no obvious deviation from the MBH-O".relation defined for inactive galaxies when the uncertainties in MBH and the luminosity bias are concerned.(2) We find that the radio-loud quasars deviate more from the MBH-σ.relation than do the radio-quiet quasars.This deviation is only partly due to a possible cosmological evolution of the MBH-σ* relation and the luminosity bias.(3) The radioluminosity is proportional to M128 0.23-0.16 BH(LBol/LEdd)1.29 0.31-0.24 for radio-quiet quasars and to M3.10 0.6.-0.70(LBol.LEdd)4.18 1.40-1.10 for radio-loud quasars.The weaker dependence of the radio luminosity on the mass and the Eddington ratio for radio-loud quasars shows that other physical effects would account for their radio luminosities,such as the spin of the black hole.