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利用平均海面推定青岛水准原点地区的地壳垂直运动 总被引:2,自引:0,他引:2
通常利用平均海面所求某点地壳垂直运动是一种视运动,如若干年平均海面实际升降变化为V,陆地实际垂直运动为U,则视垂直运动为(U-V).在推定地区地壳垂直运动,使用平均海面数据时应注意其区域性和周期性的变化.文中以有代表性的平均海面变化结果为依据,求出青岛国家水准原点地区地壳垂直运动速率λn=(+2.2±0.5)mm/a. 相似文献
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论述了数字水准仪的基本特点,基于这些特点将数字水准仪主机、条码尺和数据处理软件作为一个整体进行系统检定是一种恰当的方法。文中给出了系统检定的原理、测点数及位移量的确定方法。最后用模拟数据进行了计算,模拟计算结果表明:正确的位移量是求解尺度改正数的前提。 相似文献
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Generalization is a comprehensive process. It is not simply a question of an algorithm, such as simplification, selection, displacement, and so on. Only after geometric shapes and topological properties have been understood fully, can a sound and automated generalization process be possible. This article proposes a new theoretical model for sounding generalization in digital nautical charts. First, with the aid of Delaunay triangulation, a tree structure is introduced for a hierarchical representation of the marine topography. Then, an analytical algorithm for the recognition and the measurement of the marine topography is developed through the use of the tree structure. Finally, all of the techniques mentioned above are integrated into a model for sounding generalization, of which results are illustrated with the aid of several examples. 相似文献
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Generalization is a comprehensive process. It is not simply a question of an algorithm, such as simplification, selection, displacement, and so on. Only after geometric shapes and topological properties have been understood fully, can a sound and automated generalization process be possible. This article proposes a new theoretical model for sounding generalization in digital nautical charts. First, with the aid of Delaunay triangulation, a tree structure is introduced for a hierarchical representation of the marine topography. Then, an analytical algorithm for the recognition and the measurement of the marine topography is developed through the use of the tree structure. Finally, all of the techniques mentioned above are integrated into a model for sounding generalization, of which results are illustrated with the aid of several examples. 相似文献
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验潮站观测的海面高度数据是监测海平面变化以及确定平均海面时常使用的重要基础观测信息,针对平均海面以及相对海平面变化速率在不同时段观测资料下结果的差异进行了分析,统计了不同时间尺度平均海面确定的差异,并设计了两组数据实验,具体讨论了不同年份19年观测以及观测时长逐年累加两种情况下,相对海平面变化速率确定结果的规律。实验结果表明,月平均海面具有明显的季节性变化,最大互差可达几十厘米,1年平均海面基本稳定,19年平均海面精度可达厘米级;利用19年的观测资料确定的相对海平面变化速率反映的观测时段内海平面的变化情况,各时段结果差异较大且可靠性较低;为获得稳定可靠的相对海平面变化速率,观测时长应至少涵盖两个潮汐变化周期。 相似文献