海洋磁力测量空间归算阈值条件确定及其应用     

于波  黄谟涛  翟国君  刘雁春 《武汉大学学报(信息科学版)》2010,(2)

对仿真和实测数据的空间变化进行了分析,得出拖鱼起伏高度变化对测量成果的影响量级与测区磁异常水平梯度变化的复杂程度有关。提出了归算的阈值条件,并通过实例验证了该条件的合理性与实用性,并提出当测区要求是一级、二级和三级测量精度时,必须将测量数据归算到平均海面上。  相似文献   

疏浚中基于Matlab的土方量计算方法     

张翠峰  万计 《地理空间信息》2010,8(5):138-140

通过比较疏浚测量中计算土方量所采用的平均水深方法和不规则三角网法,结合工程实例,提出了一种基于插值运算的软件算法,并对三者进行了对比分析,得出程序算法在疏浚测量计算土方量工作中的特点和优势。  相似文献   

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罗海滨  何秀凤 《大地测量与地球动力学》2007,27(3):35-38

?????????InSAR???????????????????????????GPS????InSAR????????????????????????InSAR???????????Ч???????????SAR???????????????????????????????GPS?????????????м???????????????????巨??IDW????GPS????????????????д???????????????????????????????????????費?????????????????????IIDW????巨????????????????????????????巨?????????????????????????巨????????????????????????????????????????????????巨Ч?????á?  相似文献   

Preliminary 10Be chronology for the last deglaciation of the western margin of the Greenland Ice Sheet     

Vincent Rinterknecht  Yuri Gorokhovich  Joerg Schaefer  Marc Caffee 《第四纪科学杂志》2009,24(3):270-278

The now acknowledged thinning of the Greenland Ice Sheet raises concerns about its potential contribution to future sea level rise. In order to appreciate the full extent of its contribution to sea level rise, reconstruction of the ice sheet's most recent last deglaciation could provide key information on the timing and the height of the ice sheet at a time of rapid climate readjustment. We measured ¹⁰Be concentrations in 12 samples collected along longitudinal and altitudinal transects from Sisimiut to within 10 km of the Isunguata Sermia Glacier ice margin on the western coast of Greenland. Along the longitudinal transect, we collected three perched boulders and two bedrocks. In addition, we sampled seven perched boulders along a vertical transect in a valley within 10 km of the Isunguata Sermia Glacier ice margin. Our pilot dataset constrains the height of the ice sheet during the Last Glacial Maximum (LGM) between 500 m and 840 m (including the 120 m relative sea level depression at the time of the LGM, 21 ka BP). From the transect we estimate the thinning of the ice sheet at the end of the deglaciation between 12.3 ± 1.5 ¹⁰Be ka (n = 2) and 8.3 ± 1.2 ¹⁰Be ka (n = 3) to be ～6 cm a^?1 over this time period. Direct dating of the retreat of the western margin of the Greenland Ice Sheet has the potential to better constrain the retreat rate of the ice margin, the thickness of the former ice sheet as well as its response to climate change. Copyright © 2008 John Wiley & Sons, Ltd.  相似文献   

A HIGH-RESOLUTION, GRIDDED DATASET FOR MONTHLY TEMPERATURE NORMALS (1971-2000) IN SWEDEN     

DELIANG CHEN  LEBING GONG  CHONG-YU XU  SVEN HALLDIN 《Geografiska Annaler: Series A, Physical Geography》2007,89(4):249-261

A baseline climatology is required in evaluating climate variability and changes on regional and local scales. Gridded climate normals, i.e. averages over a 30‐year period, are of special interest since they can be readily used for validation of climate models. This study is aimed at creating an updated gridded dataset for Swedish monthly temperature normals over the period 1971–2000, based on standard 2‐m air temperature records at 510 stations in mainland Sweden. Spatial trends of the normal temperatures were modelled as functions of latitude, longitude and elevation by multiple linear regression. The study shows that the temperature normals are strongly correlated with latitude throughout the year and especially in cold months, while elevation was a more important factor in June and July. Longitude played a minor role and was only significant in April and May. Regression equations linking temperature to latitude, longitude and elevation were set up for each month. Monthly temperature normals were detrended by subtracting spatial trends given by the regressions. Ordinary kriging was then applied to both original data (simple method) and de‐trended data (composite method) to model the spatial variability and to perform spatial gridding. The multiple regressions showed that between 82% (summer) and 96% (winter) of the variance in monthly temperature normals could be explained by latitude and elevation. Unexplained variances, i.e. the residuals, were modelled with ordinary kriging with exponential semivariograms. The composite grid estimates were calculated by adding the multiple linear trends back to the interpolated residuals at each grid point. Kriged original temperature normals provided a performance benchmark. The cross–validation shows that the interpolation errors of the normals are significantly reduced if the composite method rather than the simple one was used. A gridded monthly dataset with 30‐arcsecond spacing was created using the established trends, the kriging model and a digital topographic dataset.  相似文献   

边坡临界高度卡尔曼公式之工程应用   总被引：1，自引：0，他引：1  

蒋忠信 《岩土工程技术》2007,21(5):217-220

对边坡临界高度这一工程地质和岩土工程问题,古典的卡尔曼分析法至今仍有生命力和应用价值。全面归纳了确定一般边坡、直立边坡和具张裂隙边坡的临界高度的卡尔曼公式,并提出了应用这些公式的方法和条件,以工程滑坡、路堑边坡、挡墙基坑和天然危岩为例示范了公式的工程应用。  相似文献   

基于二元样条函数的DEM传递误差模型     

王耀革  姚红 《测绘学院学报》2007,(Z1)

根据两点数值微分公式建立了基于二元样条函数的规则格网数字高程模型(DEM)的表面表达模型,得出了基于二元样条函数的传递误差公式。公式表明,二元样条函数的DEM传递误差与双线性多项式的传递误差相同。但由于样条函数的DEM表面建模误差低于线性多项式的DEM表面建模误差,因此,基于样条函数的DEM表面模型具有更高的精度。  相似文献   

我国现代高程测定关键技术若干问题的研究及进展   总被引：5，自引：0，他引：5  

李建成 《武汉大学学报(信息科学版)》2007,32(11):980-987

阐述了大地水准面在大地测量学及相关地球科学中的科学意义、作用及其应用,提出了利用GPS技术结合高精度似大地水准面代替我国高程测定的思路,分析了目前地球重力场长波、中波和短波在计算cm级大地水准面中具备的条件,论述了确定1 cm精度城市和5 cm省级似大地水准面的若干关键技术问题及其必要性和可行性,提出了我国cm级大地水准面确定中需解决的主要理论问题和若干关键技术,评述了我国局部大地水准面的主要进展和取得的成果。  相似文献   

工程放样中三角高程的精度分析     

左淑红  左凤鸣  郑丽娜 《测绘与空间地理信息》2007,30(5):148-150

三角高程放样中,平面位置放样与高程放样都采用经纬仪,是一种快速的方法,但距离误差及高差误差与竖直角有很大的关系,本文对此进行了分析。同时分析了测距仪的放样精度。  相似文献   

一种GNSS网络RTK改进的综合误差内插方法   总被引：2，自引：1，他引：2  

唐卫明  刘经南  刘晖  白清波 《武汉大学学报(信息科学版)》2007,32(12):1156-1159

在全球导航卫星系统（GNSS）网络RTK综合误差内插法（CBI）的基础上，提出了一种改进的综合误差内插方法（MCBI）。该方法把综合误差分为对流层模型改正、一阶电离层影响和除一阶电离层影响外的其他综合影响3个部分。实例证明了该方法不仅在精度上比综舍误差内插法要高，而且更利于流动站的应用。  相似文献