• 其中平均海平重合就是大地水准面

    Which coincide with the mean sea level surface is the geoid.

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  • 讨论垂直位移重力变化大地水准面变化影响

    The effects of surface vertical displacements and gravity changes upon the geoidal height variation have been also discussed.

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  • 物理大地测量主要目标确定地球外部重力场大地水准面

    The main purpose of physical geodesy is to ascertain the outer Earth gravity field and geoid.

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  • 数据分辨率影响地球重力场建模大地水准面精度重要因素。

    Data resolution has an important effect on modeling the earth's gravity field and the accuracy of the geoid.

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  • 发明公开了一种基于扰动重力的大地水准面陆海无缝拼接方法

    The invention discloses a disturbing gravity-based quasi-geoid land-sea seamless splicing method.

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  • 模型EGM96相比(70阶次),大地水准面起伏差异大为2

    The maximum difference of geoid undulation between the model and EGM96(to 70 degrees) is 2.

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  • 区域精化大地水准面全国多个地区已经建立,同时也得到了广泛应用。

    The local refined Quasi-Geoid has been constructed in several regions and widely applied.

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  • 利用TOPEX资料可以得到新的地球引力场海洋大地水准面海潮模型

    Using TOPEX altimeter data, a few new earth gravity models, geoid models and ocean tide models were generated, and these models were better than old models.

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  • 动态改变大地水准面差距地球半径比值,改善了地球形状的三维表达效果;

    Dynamic changing the scale of geoid undulations and the radius of the earth, the video mode of the earth figure is improved.

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  • 将地球位模型计算的阜新大地水准合于GPS水准实测的似大地水准面

    The quasi-geoid computed by geopotential model is fitted with the quasi-geoid measured by GPS leveling.

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  • 图上精确地球大地水准面是根据洋流海平变化地球冰川等元素的精确数据测量而成。

    A precise model of Earth's geoidis crucial for deriving accurate measurements of ocean circulation, sea-level change and terrestrial ice dynamics.

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  • 介绍统计学习理论支持向量提出利用支持向量机技术进行大地水准面拟合。

    This paper introduces statistical learning theory and support vector machine, proposes a new method, support vector machine technology, to simulate quasi-geoid.

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  • 一般说来,水准测量测出大地水准高程精度远远超过任何其它方法的精度。

    In general the accuracy of geoidal heights, as given by spirit levelling, much exceeds that of any other system.

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  • 利用成都市大地水准面模型探测分析了两个传统高程控制中可能存在系统偏差

    The systematic bias of the two traditional vertical network was detected and analyzed by use of Chengdu quasi-geoid.

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  • 这个新的大地水准面地图对于研究海洋环流海冰动力学海平变化地震有用的

    The new geoid map will be useful for studying ocean circulation, ice dynamics, sea-level change and earthquakes.

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  • 大地水准面反映研究区板块相互作用的特点,高频成分可以刻画各海盆构造特征。

    The altimetry geoid undulation is mainly conducted by convergence between two or three plates, and its components at short wavelength characterize tectonics within basins.

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  • 上精确地球大地水准面根据洋流、海平变化地球冰川等元素的精确数据测量而成。

    A precise model of Earth's geoid is crucial for deriving accurate measurements of ocean circulation, sea-level change and terrestrial ice dynamics.

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  • 采用正常拟合方法顾及了似大地水准面模型几何特性顾及物理特性。

    Residuals used in normal fitting method, not only takes into account the quasi-geoid model for the geometric properties, but also take into account its physical properties.

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  • 依据岩石圈弹性挠曲均衡补偿理论建立地形-均衡补偿重力大地水准面异常级数表达式

    Base on theory of lithosphere elastic flexure isostatic compensation, the spheric harmonic series expressions of topography-isostasy compensation gravity and geoid are established.

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  • 结果表明菲律宾南海显示了与磁条带扩张脊对应斜交的高频成分大地水准面起伏条带。

    The results show that within the Philippine Sea and the South China Sea, short - wavelength lineations of the geoid undulation are parallel or cross to magnetic lineations and rifting ridges.

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  • 影响高原山区大地水准面起伏变化主要原因地形的剧烈变化,地形量和岩石密度分布不均匀。

    The main factors to influence the Geoids rising and falling of the mountainous districts are the acute change of the landform and the asymmetry of the mass of landform and the density of rocks.

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  • 基于扼要提出应用重力大地水准几何大地水准面综合法GPS椭球化为正高的方法。

    This paper puts forward, in the point, gravimetric geoid method, geometric geoid method and synthesis method to transform ellipsoid height into orthometric height.

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  • 并利用我国河西地区1992 - 2003年的重复重力观测资料地区的大地水准面变化进行计算研究。

    He-Xi geoid's changes is calculated and researched with the gravity variation data in the period from 1992 to 2003.

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  • 另外采用阻尼最小二乘方法利用全球地震层析成像资料大地水准面异常资料联合反演了全球地幔密度异常。

    Moreover, The authors inverted three dimensional global mantle density (anomaly) combining geoid data and seismic tomography data by means of damping least square method.

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  • 长距离超高压送电线路工程GPS测量中如何选择大地水准面模型,如何确定GPS测量高程等问题进行了讨论。

    This paper has discussed how to select geoidal model and how to determine normal height in GPS survey of long distance transmission line project.

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  • 利用WDM94模型编制了华北地区不同阶次的大地水准起伏讨论了大地水准面起伏地区构造横向不均匀关系

    The geoid undulation diagrams in different degrees are mapped by WDM94 model. The relationship between the geoid undulation and the lateral inhomogeneity of regional tectonics is discussed.

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  • 利用GPS水准模拟大地水准进行约束,采用“去——恢复”技术函数进行拟内插,得到转换后的大地水准面

    The GPS-levelling is used to add constraints on the simulated geoid, and the "remove-restore" method and the multi-quadric function method are used to interpolation, so as to obtain the refined geoid.

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  • 利用GPS水准模拟大地水准进行约束,采用“去——恢复”技术函数进行拟内插,得到转换后的大地水准面

    The GPS-levelling is used to add constraints on the simulated geoid, and the "remove-restore" method and the multi-quadric function method are used to interpolation, so as to obtain the refined geoid.

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