Signal acquisition of Luojia-1A low earth orbit navigation augmentation system with software defined receiver     

Liang Chen  Xiangchen Lu  Nan Shen  Lei Wang  Yuan Zhuang  Ye Su  Deren Li  Ruizhi Chen 《地球空间信息科学学报》2022,(1):47-62

Low Earth Orbit (LEO) satellite navigation signal can be used as an opportunity signal in the case of a Global Navigation Satellite System (GNSS) outage, or as ...  相似文献   

遥感影像相对辐射校正方法及适用性研究   总被引：2，自引：1，他引：1  

段依妮  张立福  晏磊  吴太夏  刘跃生  童庆禧 《遥感学报》2014,18(3):597-617

遥感影像相对辐射校正是一项基础的数据预处理工作,用于去除影像整体的辐射不均匀性、条带噪声、坏线等辐射问题,经过30多年的发展,已形成几十种不同的相对辐射校正方法和算法。面对种类众多的相对辐射校正方法,它们之间的区别和关联是什么,每种方法的特点是什么,如何选择合适的校正方法,是3个亟需解决的问题。围绕这3个问题,第一,本文以相对辐射校正系数获取的不同方式为原则,将现有的相对辐射校正方法分为3大类:定标法、统计法和综合法,使该分类体系能够反映各类校正方法的区别和关联。第二,在新的分类体系下,给出了定标法、统计法、综合法的数学模型表达,详细介绍了3类方法包含的每种具体的校正方法和算法,比较分析了每种方法的基本思想、原理和优缺点。第三,从影像辐射不均匀特征、影像几何特征、传感器定标、影像综合特征4个方面,对各种校正方法的适用性进行综合分析,给出了科学合理地选择相对辐射校正方法的建议,同时结合具体应用实例进行了实验验证。最后,分析了相对辐射校正研究的发展趋势和存在的问题,有效信息和噪声的计算机判定准则、相对辐射校正效果的评价体系、相对辐射校正对于后续的绝对辐射校正结果的影响是下一步需要深入研究的问题。  相似文献   

嫦娥三号导航相机测图能力分析及地形重建     

彭嫚  万文辉  吴凯  刘召芹  李力  邸凯昌  李立春  苗毅  詹磊 《遥感学报》2014,18(5):995-1002

基于立体相机成像模型并结合相机参数对嫦娥三号导航相机3维测图能力进行分析,利用摄影测量原理和误差传播定律对巡视器30 m范围内的DEM精度进行了理论分析,推导出导航相机立体影像获得的采样点精度公式,并绘制了DEM的平面精度图和高程精度图;同时使用多线程技术开发了基于导航相机立体影像的地形快速重建算法,利用多线程技术完成影像的特征匹配和密集匹配,并通过分块内插生成DEM。该技术应用于嫦娥三号任务中,有力地支持了嫦娥三号遥操作路径规划相关任务。  相似文献   

福建省GPS基准站数据处理与分析     

占惠 《全球定位系统》2014,(6):61-65

利用福建省41个GPS基准站2011—2014年的观测资料,运用GAMIT／GLOBKl0．4软件及块体整体旋转线性应变模型,得到了福建省各测站及分块的水平运动速度场和块体上的应变图像。通过分析研究2011—2013和2011-2014两个时段速度场和应变场的特征,为福建省未来地震活动判定提供形变依据。  相似文献   

The Characteristics of Atmospheric Ice Nuclei Measured at Different Altitudes in the Huangshan Mountains in Southeast China简   总被引：3，自引：0，他引：3  

JIANG Hui  YIN Yan  YANG Lei  YANG Shaozhong  SU Hang  and CHEN Kui 《大气科学进展》2014,31(2):396-406

The concentration of ice nuclei （IN） and the relationship with aerosol particles were measured and analyzed using three 5-L mixing cloud chambers and a static diffusion cloud chamber at three altitudes in the Huangshan Mountains in Southeast China from May to September 2011.The results showed that the mean total number concentration of IN on the highest peak of the Huangshan Mountains at an activation temperature （Ta） of-20℃C was 16.6 L-1.When the supersaturation with respect to water （Sw） and with respect to ice （Si） were set to 5％,the average number concentrations of IN measured at an activation temperature of-20℃C by the static diffusion cloud chamber were 0.89 and 0.105 L-1,respectively.A comparison of the concentrations of IN at three different altitudes showed that the concentration of IN at the foot of the mountains was higher than at the peak.A further calculation of the correlation between IN and the concentrations of aerosol particles of different size ranges showed that the IN concentration was well correlated with the concentration of aerosol particles in the size range of 1.2-20 μtm.It was also found that the IN concentration varied with meteorological conditions,such as wind speed,with higher IN concentrations often observed on days with strong wind.An analysis of the backward trajectories of air masses showed that low IN concentrations were often related to air masses travelling along southwest pathways,while higher IN concentrations were usually related to those transported along northeast pathways.  相似文献   

大尺度环流的年代际变化对初夏华南持续性暴雨的影响   总被引：2，自引：2，他引：0  

刘蕾  孙颖  张蓬勃 《气象学报》2014,72(4):690-702

利用1961-2010年中国逐日降水数据和NCEP/NCAR逐日再分析资料集,研究了大尺度环流的年代际变化对不同频发年代华南持续性暴雨的影响。结果表明,虽然过去50年里华南持续性暴雨的发生存在两个频发时段(20世纪60年代中期到70年代中期、20世纪90年代初到2010年),其典型环流配置都表现为中高纬度冷空气和低纬度充沛水汽的配合,但不同频发时段的大尺度环流配置明显不同,这种配置使得两个频发时段的暴雨发生特点有所不同,最近20年的暴雨发生次数更多,强度更强,持续时间更长。在频发的1964-1976年,高纬度的冷空气主要来自西西伯利亚上空深厚的低槽前部,而此时南亚高压偏弱,西太平洋副热带高压偏弱、偏东,低纬度的水汽主要来自孟加拉湾印缅低压槽前,可降水量偏小,但垂直速度较大,水汽辐合较旺盛,华南上空大气环流较不稳定;在频发的1991-2010年,鄂霍次克海上空附近的高压脊活跃,高纬度冷空气主要来自高压后部,低纬度西太平洋副热带高压偏强,位置偏西,其西北侧的水汽源源不断输送到华南上空,故可降水量增多,伴随着强大的南亚高压提供的良好的高层辐散条件,华南上空垂直速度增大,水汽辐合明显,强有利的环流配置导致1991-2010年华南持续性暴雨强度更大、范围更广。因此,大气环流的年代际转型使得华南持续性暴雨发生了巨大改变,故在未来做预测时应充分考虑不同年代际环流背景场对华南持续性暴雨的重要影响。  相似文献   

Statistical Characteristics of Convective Initiation in the Beijing-Tianjin Region Revealed by Six-Year Radar Data          下载免费PDF全文

WANG Yu  HAN Lei  WANG Hongqing 《Acta Meteorologica Sinica》2014,28(6):1127-1136

Characteristics of convective initiation (CI) in the Beijing-Tianjin region during the warm season of2008-2013 are examined. A total of 38877 CI cases are identified by a thunderstorm identification, tracking, analysis, and nowcasting algorithm. CI cases are evaluated in the context of associated terrain, weather systems, and land cover properties. The spatial distribution of all CI cases shows that there are dense CI activities around the 200-m elevation, which means that convective storms are more easily triggered over foothills. From 1500-1800 to 0300-0600 BT (Beijing Time), the high-occurrence CI region tends to propagate southeastward (i.e., from mountains to plains, then to ocean). Among the four local weather systems, the Mongolian cold vortex has the highest CI frequency while the after-trough system has the lowest CI frequency. For the land cover relationships with CI, the urban land cover has the highest CI density and the forest-type land cover has the second highest CI density; these two types of land cover are more conducive to CI formation.  相似文献   

Natural variability of summer rainfall over China in HadCM3   总被引：1，自引：0，他引：1  

Yonghui Lei  Brian Hoskins  Julia Slingo 《Climate Dynamics》2014,42(1-2):417-432

Summer rainfall over China has shown decadal variability in the past half century, which has resulted in major north–south shifts in rainfall with important implications for flooding and water resource management. This study has demonstrated how multi-century climate model simulations can be used to explore interdecadal natural variability in the climate system in order to address important questions around recent changes in Chinese summer rainfall, and whether or not anthropogenic climate change is playing a role. Using a 1,000-year simulation of HadCM3 with constant pre-industrial external forcing, the dominant modes of total and interdecadal natural variability in Chinese summer rainfall have been analysed. It has been shown that these modes are comparable in magnitude and in temporal and spatial characteristics to those observed in the latter part of the twentieth century. However, despite 1,000 years of model simulation it has not been possible to demonstrate that these modes are related to similar variations in the global circulation and surface temperature forcing occurring during the latter half of the twentieth century. This may be in part due to model biases. Consequently, recent changes in the spatial distribution of Chinese summer rainfall cannot be attributed solely to natural variability, nor has it been possible to eliminate the likelihood that anthropogenic climate change has been the driving factor. It is more likely that both play a role.  相似文献   

Tree mortality in response to climate change induced drought across Beijing,China     

Xiongqing Zhang  Yuancai Lei  Yong Pang  Xianzhao Liu  Jinzeng Wang 《Climatic change》2014,124(1-2):179-190

Tree mortality in response to climate change induced drought has emerged as a global concern. Small changes of tree mortality rates can profoundly affect forest structure, composition, dynamics and ecosystem services such as carbon sequestration. Our analyses of longitudinal data from natural stands (82 plots) in Beijing showed that tree mortality rates have increased significantly over the two decades from 1986 to 2006. In contrast, recruitment rates decreased significantly over this period. The increase in overall mortality rates resulted from an increase in tree deaths dominantly attributed to changes in temperature and precipitation resulting in drier conditions across latitudes, elevations, tree species, and tree sizes. In addition, the results showed that mortality rates of Chinese pine (Pinus tabuliformis) (β ₁ ?=?0.0874) as a result of climate change induce drought were much smaller than oak (Quercus) (β ₁ ?=?0.1583).  相似文献   

结合地形因子与分层策略的喀斯特地区无人机影像分类     

贾煜  汪泓  蔡宏  张磊 《测绘通报》2022,(2):121-127

西南喀斯特山区地形起伏较大,地物分布较为破碎,致使传统的光谱特征一次分类方法的精度较低。本文基于高分辨率无人机正射影像和地形指标,充分利用无人机遥感影像空间特征、光谱特征、纹理特征及地形特征,采取面向对象CART决策树算法与分层策略提取了研究区土地覆盖类型。研究表明,结合空间地形因子和分层策略的方法减少了破碎区地物间的相干扰,故具有较高的分类精度,总体分类精度达91.2%,Kappa系数为0.87,较传统一次分类精度提高了9.8%,Kappa系数提高了0.13。该方法对西南喀斯特地区土地覆盖解译精度较好,可为土地利用监测提供参考。  相似文献