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51.
本文对惯性测量各项系统误差及异常重力场进行了分析和研究,并在此基础上建立了两种用于惯性重力测量的估算模型;模拟计算的结果表明,所建模型在原理上是可靠的,结果是令人满意的;同时,本文较为详细地分析了各项系统误差对异常重力元素估计精度的影响,对卡尔曼滤波应用中的有关问题进行了讨论。 相似文献
52.
The second vertical derivatives of gravity and magnetic potential are widely used in geophysical prospecting because of their
better resolution. On the same basis an attempt has been made to obtain the expressions for the second vertical derivative
of the electrical potential and to compute its nature for comparison. Derivative responses over a two-layered earth and also
over an anticlinal structure have been computed and it is shown that the second vertical derivative sounding could be employed
for greater accuracy in finding out the thickness of such beds or the inclination of the sides of the anticline and its depth
when compared with normal resistivity sounding 相似文献
53.
Wind tunnel experiments were carried out to measure the spatial distribution in equilibrium transport of four types of mixed sand. The flux profiles of each grain size group were calculated. It is found that the vertical distribution of mean grain size has a close relation with the grain size distribution in the sand bed. In a log-linear plot, the flux profiles of main grain size groups are all straight lines and their slopes are nearly equal. It is also found that the ratio of transport rate of each size group to the whole transport rate is directly proportional to the mass ratio of each size group in the sand bed and the proportion value is only dependent on the grain size. This harmonious law is applicable to all four types of mixed sand used in the experiment. 相似文献
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55.
The response of the Chesapeake Bay to river discharge under the influence and absence of tide is simulated with a numerical model. Four numerical experiments are examined: (1) response to river discharge only; (2) response to river discharge plus an ambient coastal current along the shelf outside the bay; (3) response to river discharge and tidal forcing; and (4) response to river discharge, tidal forcing, and ambient coastal current. The general salinity distribution in the four cases is similar to observations inside the bay. Observed features, such as low salinity in the western side of the bay, are consistent in model results. Also, a typical estuarine circulation with seaward current in the upper layer and landward current in the lower layer is obtained in the four cases. The two cases without tide produce stronger subtidal currents than the cases with tide owing to greater frictional effects in the cases with tide. Differences in salinity distributions among the four cases appear mostly outside the bay in terms of the outflow plume structure. The two cases without tide produce an upstream (as in a Kelvin wave sense) or northward branch of the outflow plume, while the cases with tide produce an expected downstream or southward plume. Increased friction in the cases with tide changes the vertical structure of outflow at the entrance to the bay and induces large horizontal variations in the exchange flow. Consequently, the outflow from the bay is more influenced by the bottom than in the cases without tide. Therefore, a tendency for a bottom-advected plume appears in the cases with tide, rather than a surface-advected plume, which develops in the cases without tide. Further analysis shows that the tidal current favors a salt balance between the horizontal and vertical advection of salinity around the plume and hinders the upstream expansion of the plume outside the bay. 相似文献
56.
Determination of Geopotential Differences between Local Vertical Datums and Realization of a World Height System 总被引:2,自引:0,他引:2
Burša Milan Kouba Jan Müller Achim Raděj Karel True Scott A. Vatrt Viliam Vojtíšková Marie 《Studia Geophysica et Geodaetica》2001,45(2):127-132
The methodology developed for connecting Local Vertical Datums (LVD) was applied to the Australian Height Datum (AHD) and the North American Vertical Datum (NAVD88). The geopotential values at AHD and NAVD88 were computed and the corresponding vertical offset of 974 mm with rms 51 mm was obtained between the zero reference surfaces defined by AHD and NAVD88. The solution is based on the four primary geodetic parameters, the GPS/levelling sites and the geopotential model EGM96. The Global Height System (or the Major Vertical Datum) can be defined by a geoidal geopotential value used in the solution as the reference value, or by the geopotential value of the LVD, e.g. NAVD88. 相似文献
57.
58.
青藏高原北侧地区干湿年夏季垂直环流差异的对比分析及青藏高原的热力影响 总被引:30,自引:2,他引:30
为了分析西北干旱的形成原因,本文首先利用高原北侧地区5站历年夏季的降水量资料等,制定了该区的干湿标准,划分了历年夏季的干湿等级。接着又利用ECMWF的格点资料等对比分析了该区干湿年夏季间垂直环流的差异,也探讨了青藏高原地面热状况与高原北侧干湿状况的联系。其主要结论是:1)文中制定的以降水标准差为判据的干湿标准适合西北干旱区;2)高原北侧干湿年夏季间在高原北侧和高原上的垂直环流存在明显差异;3)青藏高原地面热状况与上列差异有关,也即青藏高原的热力作用是西北干旱的重要成因之一。 相似文献
59.
使用一枚携带chaff的火箭观测到的垂直速度数据,研究中层大气垂直速度扰动细微结构。结果表明,垂直速度扰动有明显的层状结构,各层厚度约150-500m,层间垂直分离距离在几百米到1-3km间。在垂直速度方差和低Ri数峰值间以及动力不稳定和MST雷达回波区域间有好的对应关系。水平速度垂直波数谱与饱和谱在谱斜率和谱振幅上存在好的一致.这些观测结果表明,火箭测量到的细微结构可以用波场饱和解释。 相似文献
60.
本文介绍了葛洲坝垂直位移遥控监测系统的工作原理、结构、电路设计特点及实际使用效果。几年的实测结果证明了此系统量测精度高、稳定性好、自动化程度高,实现了联机实时自动监测大坝垂直位移的目标。 相似文献